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	{"id":3292,"date":"2021-07-05T13:23:27","date_gmt":"2021-07-05T10:23:27","guid":{"rendered":"https:\/\/www.lemnosgeomonuments.gr\/%cf%87%ce%ac%cf%81%cf%84%ce%b7%cf%82\/"},"modified":"2022-03-24T13:32:48","modified_gmt":"2022-03-24T11:32:48","slug":"%cf%87%ce%ac%cf%81%cf%84%ce%b7%cf%82","status":"publish","type":"page","link":"https:\/\/www.lemnosgeomonuments.gr\/en\/%cf%87%ce%ac%cf%81%cf%84%ce%b7%cf%82\/","title":{"rendered":"Interactive map"},"content":{"rendered":"<p>[et_pb_section fb_built=&#8221;1&#8243; disabled_on=&#8221;off|off|off&#8221; admin_label=&#8221;Events&#8221; _builder_version=&#8221;4.9.7&#8243; background_color=&#8221;#5e8777&#8243; custom_padding=&#8221;||0|0px|false|false&#8221; custom_width_px__hover=&#8221;1080px&#8221; custom_width_px__hover_enabled=&#8221;1080px&#8221; custom_width_percent__hover=&#8221;80%&#8221; custom_width_percent__hover_enabled=&#8221;80%&#8221; global_colors_info=&#8221;{}&#8221; gutter_width__hover=&#8221;3&#8243; 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src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039c\\u039f\\u03a5\\u03a3\\u0395\\u0399\\u039f-\\u039d\\u0391\\u03a5\\u03a4\\u0399\\u039a\\u0397\\u03a3-\\u03a0\\u0391\\u03a1\\u0391\\u0394\\u039f\\u03a3\\u0397\\u03a3-\\u039a\\u0391\\u0399-\\u03a3\\u03a0\\u039f\\u0393\\u0393\\u0391\\u039b\\u0399\\u0395\\u0399\\u0391\\u03a3_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/museum-of-maritime-tradition-nea-koutali\\\/\\\">Museum of Maritime Tradition (Nea Koutali)<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/museum-of-maritime-tradition-nea-koutali\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Address: Municipality of Lemnos, Lemnos, PC 81400 Opening Hours: Summer Season (1\\\/7 to 31\\\/8) Daily 10:00 - 14:00 &amp; 19.00 - 21.00 Sundays - Holidays: 10.30 - 14.30 Closed on Monday Winter season (1\\\/9 to 30\\\/6) By appointment Telephone: (+30) 22540 92383 (Museum), (+30) 22543 50024 (Municipality of Lemnos) Mobile: (+30) 6978947557 Fax: 22540 92383 [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8934\",\"lng\":\"25.2031\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/museum-of-maritime-tradition-nea-koutali\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Address: Municipality of Lemnos, Lemnos, PC 81400 Opening Hours: Summer Season (1\\\/7 to 31\\\/8) Daily 10:00 - 14:00 &amp; 19.00 - 21.00 Sundays - Holidays: 10.30 - 14.30 Closed on Monday Winter season (1\\\/9 to 30\\\/6) By appointment Telephone: (+30) 22540 92383 (Museum), (+30) 22543 50024 (Municipality of Lemnos) Mobile: (+30) 6978947557 Fax: 22540 92383 [&hellip;]<\\\/p>\\n\",\"post_content\":\"Address: Municipality of Lemnos, Lemnos, PC 81400\\r\\nOpening Hours: Summer Season (1\\\/7 to 31\\\/8)\\r\\nDaily 10:00 - 14:00 &amp; 19.00 - 21.00\\r\\nSundays - Holidays: 10.30 - 14.30\\r\\n\\r\\nClosed on Monday\\r\\n\\r\\nWinter season (1\\\/9 to 30\\\/6) By appointment\\r\\nTelephone: (+30) 22540 92383 (Museum), (+30) 22543 50024 (Municipality of Lemnos)\\r\\nMobile: (+30) 6978947557\\r\\nFax: 22540 92383\\r\\n\\r\\nThe Museum of Maritime Tradition is the result of approximately forty years of hard work by the residents of Nea Koutali. It was established in 1996 on the initiative of the Nea Koutali Community Council, chaired by Giannis Moschovakis. The Community of Nea Koutali carried out the building\\u2019s expansion and general design of the display units which were finished in 2006 by the Kapodistrian Municipality of N. Koutalis, under the mayorship of Dimitrios Voulgarakis.\\u00a0 The construction of the museum was funded by the community of Nea Koutali, the Municipality of Nea Koutali, the inheritance of Georgios Petridis and the European Initiative \\u201cLeader\\u201d. Once a community space that was used as a community clinic, the renovated building now houses the museum\\u2019s archeological and modern artifact collection. 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of Contemporary Art (Kontias)\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Gallery of Contemporary Art (Kontias)\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u0399\\u039d\\u0391\\u039a\\u039f\\u0398\\u0397\\u039a\\u0397-\\u03a3\\u03a5\\u0393\\u03a7\\u03a1\\u039f\\u039d\\u0397\\u03a3-\\u0392\\u0391\\u039b\\u039a\\u0391\\u039d\\u0399\\u039a\\u0397\\u03a3-\\u03a4\\u0395\\u03a7\\u039d\\u0397\\u03a3_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/gallery-of-contemporary-art-kontias\\\/\\\">Gallery of Contemporary Art (Kontias)<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/gallery-of-contemporary-art-kontias\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Address: Kontias Lemnou, 81400 Working hours: June: every day, 10: 00-14: 00, Tuesday closed July, August: every day, 10: 00-14: 00, 19: 00-21: 00, Tuesday closed September: every day, 10: 00-14: 00, Tuesday closed Telephone: 2254051425 Email: info@pinakothikikondia.gr Established in 2007, the Gallery of Contemporary Balkan Art exhibits works by Balkan artists. The concept began [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8633\",\"lng\":\"25.1482\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/gallery-of-contemporary-art-kontias\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Address: Kontias Lemnou, 81400 Working hours: June: every day, 10: 00-14: 00, Tuesday closed July, August: every day, 10: 00-14: 00, 19: 00-21: 00, Tuesday closed September: every day, 10: 00-14: 00, Tuesday closed Telephone: 2254051425 Email: info@pinakothikikondia.gr Established in 2007, the Gallery of Contemporary Balkan Art exhibits works by Balkan artists. The concept began [&hellip;]<\\\/p>\\n\",\"post_content\":\"Address: Kontias Lemnou, 81400\\r\\nWorking hours:\\r\\nJune: every day, 10: 00-14: 00, Tuesday closed\\r\\nJuly, August: every day, 10: 00-14: 00, 19: 00-21: 00, Tuesday closed\\r\\nSeptember: every day, 10: 00-14: 00, Tuesday closed\\r\\nTelephone: 2254051425\\r\\nEmail: <a href=\\\"mailto:info@pinakothikikondia.gr\\\">info@pinakothikikondia.gr<\\\/a>\\r\\n\\r\\nEstablished in 2007, the Gallery of Contemporary Balkan Art exhibits works by Balkan artists.\\r\\n\\r\\nThe concept began about 10 years ago when members of the Cultural Association of Kondias of Lemnos, who were active in the traditional village of Kontias, decided to hold a Balkan art symposium. 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Since however then the gallery has hosted periodic exhibitions of well-known names from the art world, as well as new artists - and even students.\\r\\n\\r\\nThe Gallery of Contemporary Balkan Art Kontia is housed in a rebuilt traditional stone Lemnian building.\",\"post_title\":\"Gallery of Contemporary Art (Kontias)\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/gallery-of-contemporary-art-kontias\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Gallery of Contemporary Art (Kontias)\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u0399\\u039d\\u0391\\u039a\\u039f\\u0398\\u0397\\u039a\\u0397-\\u03a3\\u03a5\\u0393\\u03a7\\u03a1\\u039f\\u039d\\u0397\\u03a3-\\u0392\\u0391\\u039b\\u039a\\u0391\\u039d\\u0399\\u039a\\u0397\\u03a3-\\u03a4\\u0395\\u03a7\\u039d\\u0397\\u03a3_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"9\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.8633\",\"%_wpgmp_metabox_longitude%\":\"25.1482\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%wpcf-latitude%\":\"\",\"%wpcf-longtitude%\":\"\",\"%wpcf-location%\":\"\",\"%wpcf-code%\":\"\",\"%wpcf-mapicon%\":\"\",\"%_wpml_location_migration_done%\":\"1\",\"%_wpml_word_count%\":\"{\\\"total\\\":242,\\\"to_translate\\\":{\\\"en\\\":242}}\",\"%_thumbnail_id%\":\"2938\",\"%_edit_lock%\":\"1674655546:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%80%ce%b9%ce%bd%ce%b1%ce%ba%ce%bf%ce%b8%ce%ae%ce%ba%ce%b7-%cf%83%cf%8d%ce%b3%cf%87%cf%81%ce%bf%ce%bd%ce%b7%cf%82-%cf%84%ce%ad%cf%87%ce%bd%ce%b7%cf%82-%ce%ba%ce%bf%ce%bd%cf%84%ce%b9%ce%ac%cf%82\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u0399\\u039d\\u0391\\u039a\\u039f\\u0398\\u0397\\u039a\\u0397-\\u03a3\\u03a5\\u0393\\u03a7\\u03a1\\u039f\\u039d\\u0397\\u03a3-\\u0392\\u0391\\u039b\\u039a\\u0391\\u039d\\u0399\\u039a\\u0397\\u03a3-\\u03a4\\u0395\\u03a7\\u039d\\u0397\\u03a3_001.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"22417\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u0399\\u039d\\u0391\\u039a\\u039f\\u0398\\u0397\\u039a\\u0397-\\u03a3\\u03a5\\u0393\\u03a7\\u03a1\\u039f\\u039d\\u0397\\u03a3-\\u0392\\u0391\\u039b\\u039a\\u0391\\u039d\\u0399\\u039a\\u0397\\u03a3-\\u03a4\\u0395\\u03a7\\u039d\\u0397\\u03a3_001.jpg, \\u03a0\\u0399\\u039d\\u0391\\u039a\\u039f\\u0398\\u0397\\u039a\\u0397 \\u03a3\\u03a5\\u0393\\u03a7\\u03a1\\u039f\\u039d\\u0397\\u03a3 \\u0392\\u0391\\u039b\\u039a\\u0391\\u039d\\u0399\\u039a\\u0397\\u03a3 \\u03a4\\u0395\\u03a7\\u039d\\u0397\\u03a3_001, \",\"%_et_pb_truncate_post%\":\"<p>Address: Kontias Lemnou, 81400<br \\\/>\\nWorking hours:<br \\\/>\\nJune: every day, 10: 00-14: 00, Tuesday closed<br \\\/>\\nJuly, August: every day, 10: 00-14: 00, 19: 00-21: 00, Tuesday closed<br \\\/>\\nSeptember: every day, 10: 00-14: 00, Tuesday closed<br \\\/>\\nTelephone: 2254051425<br \\\/>\\nEmail: info@pinakothikikondia.gr<\\\/p>\\n<p>Established in 2007, the Gallery of Contemporary Balkan Art exhibits works by Balkan artists.<\\\/p>\\n<p>The concept began about 10 years ago when members of the Cultural Association of Kondias of Lemnos, who were active in the traditional village of Kontias, decided to hold a Balkan art symposium. The First Symposium was held in Kontias in 1999, opening the way for the eventual establishment of the Kontias Gallery of Contemporary Balkan Art.<\\\/p>\\n<p>Artists from Greece, Albania, Bulgaria, Montenegro, Romania, Serbia, FYROM, and Turkey created artwork and taught young islanders before donating their work to the organization. The symposium was repeated with even greater success in 2001, setting the foundation for the establishment of the Kontia Gallery of Contemporary Balkan Art. The collection at the Kontia Gallery of Contemporary Balkan Art was once focused on Lemnos-themed works and the ways in which the island is portrayed by the great Balkan artists. 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class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Atsiki\\\" width=\\\"300\\\" height=\\\"221\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u03a4\\u03a3\\u0399\\u039a\\u0397_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/atsiki\\\/\\\">Atsiki<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/atsiki\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The village's name is derived from a variation of the ancient name Attica, suggesting\\u00a0the existence of an ancient settlement there. Another theory is that the name comes from the Turkish \\\"atsik: open (place)\\\" because of the large plain that surrounds it. However, the name has been referred to since the 13th century, long before the [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9457\",\"lng\":\"25.2229\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/atsiki\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The village's name is derived from a variation of the ancient name Attica, suggesting\\u00a0the existence of an ancient settlement there. Another theory is that the name comes from the Turkish \\\"atsik: open (place)\\\" because of the large plain that surrounds it. However, the name has been referred to since the 13th century, long before the [&hellip;]<\\\/p>\\n\",\"post_content\":\"The village's name is derived from a variation of the ancient name Attica, suggesting\\u00a0the existence of an ancient settlement there. Another theory is that the name comes from the Turkish \\\"atsik: open (place)\\\" because of the large plain that surrounds it. However, the name has been referred to since the 13th century, long before the Turks arrived on Lemnos.\\r\\n\\r\\nAtsiki is home to notable writers and artists: Ioannis Fotiadis, an outstanding stone sculptor from Asia Minor, Panagiotis Haranis, sometimes known as Peter Charanis, was the rector of Byzantine studies in the United States from 1908 to 1986, Tassos Kapsidelis (1913-87), a sharp old-school historian and philologist who published four key historical volumes about Lemnos, Dr. Stavros Tragaras, painter, poet, and the heart and spirit of the Athens Association of Atsiki People, with notable efforts such as the publication of \\\"The Voice of Atsiki,\\\" the organisation of thematic seminars for Atsiki academics and workers, and the marketing of cotton, and \\u00a0George Tsimouris, a sociology professor at Panteion University, who has researched the mass migration from Asia Minor to the villages of Lemnos, as well as their manners and traditions.\\r\\n\\r\\nThe Church of Saint Giorgios, which has a stone-carved bell tower, is in Atsiki, as is the beach of Saint Ermolaou (Agiarmola) with its rare rocks.\",\"post_title\":\"Atsiki\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/atsiki\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Atsiki\\\" width=\\\"300\\\" height=\\\"221\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u03a4\\u03a3\\u0399\\u039a\\u0397_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.9457\",\"%_wpgmp_metabox_longitude%\":\"25.2229\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"10\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%wpcf-latitude%\":\"39.9457\",\"%wpcf-longtitude%\":\"25.2229\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses-1.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2975\",\"%_edit_lock%\":\"1674653464:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%b1%cf%84%cf%83%ce%b9%ce%ba%ce%ae\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"\",\"%_wpcf-image-gallery-sort-order%\":\"22728\",\"%wpcf-code%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u03a4\\u03a3\\u0399\\u039a\\u0397_001.jpg, \\u0391\\u03a4\\u03a3\\u0399\\u039a\\u0397_001, \",\"%_et_pb_truncate_post%\":\"<p>The village&#8217;s name is derived from a variation of the ancient name Attica, suggesting\\u00a0the existence of an ancient settlement there. Another theory is that the name comes from the Turkish &#8220;atsik: open (place)&#8221; because of the large plain that surrounds it. However, the name has been referred to since the 13th century, long before the Turks arrived on Lemnos.<\\\/p>\\n<p>Atsiki is home to notable writers and artists: Ioannis Fotiadis, an outstanding stone sculptor from Asia Minor, Panagiotis Haranis, sometimes known as Peter Charanis, was the rector of Byzantine studies in the United States from 1908 to 1986, Tassos Kapsidelis (1913-87), a sharp old-school historian and philologist who published four key historical volumes about Lemnos, Dr. Stavros Tragaras, painter, poet, and the heart and spirit of the Athens Association of Atsiki People, with notable efforts such as the publication of &#8220;The Voice of Atsiki,&#8221; the organisation of thematic seminars for Atsiki academics and workers, and the marketing of cotton, and \\u00a0George Tsimouris, a sociology professor at Panteion University, who has researched the mass migration from Asia Minor to the villages of Lemnos, as well as their manners and traditions.<\\\/p>\\n<p>The Church 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Tuesday closed. Summer: From Wednesday to Monday open: 08:30 - 15:30, from 14\\\/5 to 31-10-2021. Tuesday closed. Telephone: 22540 22990, 22540 22637 Email: aml@culture.gr The Archaeological Museum of Lemnos, located near the Roman Gialos Port [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8805\",\"lng\":\"25.0622\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/archaeological-museum-of-lemnos-myrina\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Address: Admiral Koundouriotis, Myrina 81400 Opening Hours: Winter: From Wednesday to Monday open: 08:30 - 15:30, from 1\\\/11\\\/2020 to 31-3-2021. Tuesday closed. Summer: From Wednesday to Monday open: 08:30 - 15:30, from 14\\\/5 to 31-10-2021. Tuesday closed. Telephone: 22540 22990, 22540 22637 Email: aml@culture.gr The Archaeological Museum of Lemnos, located near the Roman Gialos Port [&hellip;]<\\\/p>\\n\",\"post_content\":\"Address: Admiral Koundouriotis, Myrina 81400\\r\\nOpening Hours: Winter: From Wednesday to Monday open: 08:30 - 15:30, from 1\\\/11\\\/2020 to 31-3-2021. Tuesday closed.\\r\\nSummer: From Wednesday to Monday open: 08:30 - 15:30, from 14\\\/5 to 31-10-2021. Tuesday closed.\\r\\nTelephone: 22540 22990, 22540 22637\\r\\nEmail: <a href=\\\"mailto:aml@culture.gr\\\">aml@culture.gr<\\\/a>\\r\\n\\r\\nThe Archaeological Museum of Lemnos, located near the Roman Gialos Port of Myrina, exhibits the finds in Myrina of the then 20th\\u00a0Ephorate of Prehistoric and Classical Antiquities, and the Italian Archaeological School of Athens in Poliochni, Hepheastion, and Kaverio. 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Tuesday closed.<br \\\/>\\nSummer: From Wednesday to Monday open: 08:30 &#8211; 15:30, from 14\\\/5 to 31-10-2021. Tuesday closed.<br \\\/>\\nTelephone: 22540 22990, 22540 22637<br \\\/>\\nEmail: aml@culture.gr<\\\/p>\\n<p>The Archaeological Museum of Lemnos, located near the Roman Gialos Port of Myrina, exhibits the finds in Myrina of the then 20th\\u00a0Ephorate of Prehistoric and Classical Antiquities, and the Italian Archaeological School of Athens in Poliochni, Hepheastion, and Kaverio. It also includes exhibits from Lemnos artifacts, donations from private collections, and antiquities from Imvros, which were preserved by the metropolitan of Imbros Joachim just before the Asia Minor disaster. The antiquities are on display in a building from the Turkocratic period which was granted to the State by the Pallimnia School Fund to house the Archaeological Museum of Lemnos. 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Museum of the Holy Metropolis of Lemnos (Myrina)\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Ecclesiastical Museum of the Holy Metropolis of Lemnos (Myrina)\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0395\\u039a\\u039a\\u039b\\u0397\\u03a3\\u0399\\u0391\\u03a3\\u03a4\\u0399\\u039a\\u039f-\\u039c\\u039f\\u03a5\\u03a3\\u0395\\u0399\\u039f-\\u0399\\u0395\\u03a1\\u0391\\u03a3-\\u039c\\u0397\\u03a4\\u03a1\\u039f\\u03a0\\u039f\\u039b\\u0395\\u03a9\\u03a3_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/ecclesiastical-museum-of-the-holy-metropolis-of-lemnos-myrina\\\/\\\">Ecclesiastical Museum of the Holy Metropolis of Lemnos (Myrina)<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/ecclesiastical-museum-of-the-holy-metropolis-of-lemnos-myrina\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Address: Myrina, Lemnos, PC 81400 Opening Hours: 09: 00-13: 00 daily Metropolitan Telephone: 22540-24630 Office Telephone: 22540-22474 Fax: 22540-24042 The Lemnian Ecclesiastical Museum\\u00a0\\u00a0 is on the ground floor of the Metropolitan Court which can be found in the Roman 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Archbishop of Lemnos Hierotheos envisioned the project [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8807\",\"lng\":\"25.0631\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/ecclesiastical-museum-of-the-holy-metropolis-of-lemnos-myrina\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Address: Myrina, Lemnos, PC 81400 Opening Hours: 09: 00-13: 00 daily Metropolitan Telephone: 22540-24630 Office Telephone: 22540-22474 Fax: 22540-24042 The Lemnian Ecclesiastical Museum\\u00a0\\u00a0 is on the ground floor of the Metropolitan Court which can be found in the Roman Gialos port area of Myrina near the Archaeological Museum. Archbishop of Lemnos Hierotheos envisioned the project [&hellip;]<\\\/p>\\n\",\"post_content\":\"Address: Myrina, Lemnos, PC 81400\\r\\nOpening Hours: 09: 00-13: 00 daily\\r\\nMetropolitan Telephone: 22540-24630\\r\\nOffice Telephone: 22540-22474 Fax: 22540-24042\\r\\n\\r\\nThe Lemnian Ecclesiastical Museum\\u00a0\\u00a0 is on the ground floor of the Metropolitan Court which can be found in the Roman Gialos port area of Myrina near the Archaeological Museum.\\r\\n\\r\\nArchbishop of Lemnos Hierotheos envisioned the project in 1989 and brought it to completion two years later. The Lemnos Ecclesiastical Museum gathers, protects, and restores ancient sacred icons, holy artifacts, books, records, and vestments from temples and chapels on Lemnos and Agios Efstratios. 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Museum (Portianou)\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Folklore Museum (Portianou)\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039b\\u0391\\u039f\\u0393\\u03a1\\u0391\\u03a6\\u0399\\u039a\\u039f-\\u039c\\u039f\\u03a5\\u03a3\\u0395\\u0399\\u039f-\\u03a0\\u039f\\u03a1\\u03a4\\u0399\\u0391\\u039d\\u039f\\u03a5_003-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/folklore-museum-portianou\\\/\\\">Folklore Museum (Portianou)<\\\/a><\\\/div>\\r\\n            <div 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The mansion of Vagiakos was bought by Vassilis Poriazis, head of the Association of Portians of Lemnos, Athens, Piraeus, and regions. The museum's goal is to be a place where older generations can reminisce about [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8819\",\"lng\":\"25.1792\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/folklore-museum-portianou\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Address: Portianou, 81400 Opening Hours: Daily 10.00-14.00 except Tuesday Telephone: 22540 51785 The Portianos Folklore Museum was established in 1995. The mansion of Vagiakos was bought by Vassilis Poriazis, head of the Association of Portians of Lemnos, Athens, Piraeus, and regions. 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The mansion of Vagiakos was bought by Vassilis Poriazis, head of the Association of Portians of Lemnos, Athens, Piraeus, and regions.<\\\/p>\\n<p>The museum&#8217;s goal is to be a place where older generations can reminisce about their youth, and the younger generations can learn about the life of their forefathers.<\\\/p>\\n<p>The historic building housing the folklore collection has been designated a protected monument and is a remarkable example of Lemnos folk architecture.<\\\/p>\\n<p>The exhibition takes up two levels of the current structure and the ground floor of the outdoor space, covering approximately 225 square meters.<\\\/p>\\n<p>Through the selection and exhibition of historical artefacts, the main spaces of the museum seek to draw visitors back in time into the way of life of its citizens in former periods.<\\\/p>\\n<p>The methods for displaying the artefacts were chosen after researching and assessing the contents of the collection. 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Koutali\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Nea Koutali\\\" width=\\\"300\\\" height=\\\"150\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039d\\u0395\\u0391-\\u039a\\u039f\\u03a5\\u03a4\\u0391\\u039b\\u0397_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/nea-koutali\\\/\\\">Nea Koutali<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/nea-koutali\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>In 1926, Nea Koutali was built on the site of Agia Marina on the northern slope of Strompolithos, to house refugees from Koutali of Propontis. Along with Agios Dimitrios, Nea Koutali is the second settlement on Lemnos constructed by immigrants from Asia Minor. Amphitheatrically constructed along the slope near the coast of Moudros, Nea Koutali [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8937\",\"lng\":\"25.1973\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/nea-koutali\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>In 1926, Nea Koutali was built on the site of Agia Marina on the northern slope of Strompolithos, to house refugees from Koutali of Propontis. Along with Agios Dimitrios, Nea Koutali is the second settlement on Lemnos constructed by immigrants from Asia Minor. Amphitheatrically constructed along the slope near the coast of Moudros, Nea Koutali [&hellip;]<\\\/p>\\n\",\"post_content\":\"In 1926, Nea Koutali was built on the site of Agia Marina on the northern slope of Strompolithos, to house refugees from Koutali of Propontis. 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Along with Agios Dimitrios, Nea Koutali is the second settlement on Lemnos constructed by immigrants from Asia Minor.<\\\/p>\\n<p>Amphitheatrically constructed along the slope near the coast of Moudros, Nea Koutali is known\\u00a0for its excellent town planning.\\u00a0It stretches from the Agia Triada pine forest planted by refugees to the gorgeous harbor built of stone, filled with fishing boats and vessels. Nea Koutali is well-known for its sponge divers both in Greece and worldwide. The &#8220;Museum of Maritime Tradition and Sponge Fishing&#8221; opened on July 1, 2006.<\\\/p>\\n<p>Panagis Koutalianos, a prominent wrestler and weightlifter during the decade 1882-1892, made Koutali famous around the world. He was a great sailor who became famous in the United States after defeating several high-profile wrestlers of the day. 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class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kaspakas\\\/\\\">Kaspakas<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kaspakas\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The settlement was named after the Byzantine admiral Kaspakas, who lived during the reign of Alexios I Komnenos (1081-1118). The town formed an autonomous community in 1918, and Agios Ioannis and Gali have been listed as distinct settlements since 1981. In recent years, Agios Ioannis, with its sandy beach and unusual rocks, and Meteora of [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9138\",\"lng\":\"25.0817\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kaspakas\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The settlement was named after the Byzantine admiral Kaspakas, who lived during the reign of Alexios I Komnenos (1081-1118). The town formed an autonomous community in 1918, and Agios Ioannis and Gali have been listed as distinct settlements since 1981. In recent years, Agios Ioannis, with its sandy beach and unusual rocks, and Meteora of [&hellip;]<\\\/p>\\n\",\"post_content\":\"The settlement was named after the Byzantine admiral Kaspakas, who lived during the reign of Alexios I Komnenos (1081-1118). 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fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/platis\\\/\\\">Platis<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/platis\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The settlement was called after either the flat plain on which it is situated or the broad opening of the surrounding bay (wide beach), which has been used as a port since the Middle Ages. 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According to one story, the name was derived from Ag. Dimitriou's village called Kourouni. Many of the island's benefactors, primarily Egyptian immigrants, are from here. The most renowned was Odysseas I. Pantelidis, whose money [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9181\",\"lng\":\"25.1162\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kornos\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The name of the community was derived from the tap (= fountain) that existed in the town and its plentiful waters. According to one story, the name was derived from Ag. Dimitriou's village called Kourouni. Many of the island's benefactors, primarily Egyptian immigrants, are from here. The most renowned was Odysseas I. Pantelidis, whose money [&hellip;]<\\\/p>\\n\",\"post_content\":\"The name of the community was derived from the tap (= fountain) that existed in the town and its plentiful waters. 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The residents of Lera had preserved the following tradition regarding the origin of their village's name. Once upon a time, two brothers, one from Plaka and the other from Kastro, acquired Lemnos from [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9122\",\"lng\":\"25.1493\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/saint-dimitrios\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Refugees from Reisdere in Erythraia, Asia Minor, founded the settlement after 1922 on the site of Lera, a former small Turkish settlement. The residents of Lera had preserved the following tradition regarding the origin of their village's name. Once upon a time, two brothers, one from Plaka and the other from Kastro, acquired Lemnos from [&hellip;]<\\\/p>\\n\",\"post_content\":\"Refugees from Reisdere in Erythraia, Asia Minor, founded the settlement after 1922 on the site of Lera, a former small Turkish settlement. The residents of Lera had preserved the following tradition regarding the origin of their village's name. Once upon a time, two brothers, one from Plaka and the other from Kastro, acquired Lemnos from their lord father.\\u00a0 The brothers chose to divide the island at the place where they would meet, beginning each from their own town as soon as the roosters crowed. The one that began from Plaka, however, left earlier and covered more ground. His brother saw the deception as soon as they met and referred to him as \\\"filthy.\\\" As a result, the gathering place was given the name Lera. 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Pirate invasions, however, forced the residents to move to the low Karpas hill to the east of central large plain. The origin of [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9344\",\"lng\":\"25.2290\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/karpasi\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>According to local tradition, the village used to be located on the plain where the airport currently stands, specifically in the area of Trohalomandra, where ruins of houses can still be found. Pirate invasions, however, forced the residents to move to the low Karpas hill to the east of central large plain. The origin of [&hellip;]<\\\/p>\\n\",\"post_content\":\"According to local tradition, the village used to be located on the plain where the airport currently stands, specifically in the area of Trohalomandra, where ruins of houses can still be found. 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fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/varos\\\/\\\">Varos<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/varos\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The name of the region dates back to the 15th century and is of unclear origin. The town used to be located 500 metres southwest of where it is now, on the slope of the hill \\\"St'vanos,\\\" opposite the harbour of Moudros, where the settlement of\\u00a0Anemoessa now stands. The residents moved\\u00a0to the valley between the [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9296\",\"lng\":\"25.2603\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/varos\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The name of the region dates back to the 15th century and is of unclear origin. The town used to be located 500 metres southwest of where it is now, on the slope of the hill \\\"St'vanos,\\\" opposite the harbour of Moudros, where the settlement of\\u00a0Anemoessa now stands. The residents moved\\u00a0to the valley between the [&hellip;]<\\\/p>\\n\",\"post_content\":\"The name of the region dates back to the 15th century and is of unclear origin. The town used to be located 500 metres southwest of where it is now, on the slope of the hill \\\"St'vanos,\\\" opposite the harbour of Moudros, where the settlement of\\u00a0Anemoessa now stands. The residents moved\\u00a0to the valley between the hills Plagia and Lagada because of the threat of pirates. The \\\"Despotis\\\" hill stands above the settlement and is said to have been named after the island's governor, who had the title \\\"Despot of Lemnos\\\" in the late Byzantine period and supervised the area's\\u00a0mines.\\u00a0The\\u00a0remains of a volcanic crater are visible in the area, which has been linked to the old volcano Mosychlos. 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Settlements\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\"},\"id\":3719,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\",\"name\":\"\\u039f\\u03b9\\u03ba\\u03b9\\u03c3\\u03bc\\u03bf\\u03af\",\"id\":\"10\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Kallithea\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Kallithea\\\" width=\\\"300\\\" height=\\\"160\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u0391\\u039b\\u039b\\u0399\\u0398\\u0395\\u0391_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kallithea\\\/\\\">Kallithea<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kallithea\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Sarpi was the original name of the village located in the heart of the island. Amphitheatrically constructed on the slope of a low hill about 800 metres from Moudros Bay, the village offers stunning views to its inhabitants. Thus it was renamed \\\"Kallithea\\\" (good view) in 1955, as the former name was deemed Turkish. Sharpin, [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9023\",\"lng\":\"25.2072\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kallithea\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Sarpi was the original name of the village located in the heart of the island. Amphitheatrically constructed on the slope of a low hill about 800 metres from Moudros Bay, the village offers stunning views to its inhabitants. Thus it was renamed \\\"Kallithea\\\" (good view) in 1955, as the former name was deemed Turkish. Sharpin, [&hellip;]<\\\/p>\\n\",\"post_content\":\"Sarpi was the original name of the village located in the heart of the island. Amphitheatrically constructed on the slope of a low hill about 800 metres from Moudros Bay, the village offers stunning views to its inhabitants. Thus it was renamed \\\"Kallithea\\\" (good view) in 1955, as the former name was deemed Turkish. Sharpin, on the other hand, is cited in a 1361 inventory document from the Great Lavra monastery. As a result, Sharpin cannot be Turkish. Its origins are ancient, and it is one of the few Mycenaean town names that have remained on Lemnos. In particular, the term \\\"sa-pi-de: box\\\" appears in Mycenaean inscriptions, from which the ancient words \\\"sarpis (the)\\\" and \\\"sarpos (the): ark\\\" derived, and thus: \\\"wooden home.\\\" The settlement was once located further east, in the harbour of \\\"Agios Georgios,\\\" but residents were forced to relocate due to pirate threats on the one hand and swampy land on the other.\\r\\n\\r\\nThe \\\"Palaiological School of Sarpi\\\" opened in the village in 1868, the island's first peer run school outside of the capital. With the help of the devout locals,\\u00a0the church of Agios Georgios was built from the ground up in 1868. It is built in the form of a basilica, and the woodwork of the ladies area, as well as hagiographies by Pavlos Thomas (1870), Efstratios Imbrios, and Grigorios Papamalis (1918-23) are impressive.\",\"post_title\":\"Kallithea\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kallithea\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Kallithea\\\" width=\\\"300\\\" height=\\\"160\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u0391\\u039b\\u039b\\u0399\\u0398\\u0395\\u0391_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"10\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.9023\",\"%_wpgmp_metabox_longitude%\":\"25.2072\",\"%wpcf-latitude%\":\"39.9023\",\"%wpcf-longtitude%\":\"25.2072\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses-1.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2923\",\"%_edit_lock%\":\"1658148722:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%ba%ce%b1%ce%bb%ce%bb%ce%b9%ce%b8%ce%ad%ce%b1\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"\",\"%_wpcf-image-gallery-sort-order%\":\"22836\",\"%wpcf-code%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u0391\\u039b\\u039b\\u0399\\u0398\\u0395\\u0391_001.jpg, \\u039a\\u0391\\u039b\\u039b\\u0399\\u0398\\u0395\\u0391_001, \",\"%_et_pb_truncate_post%\":\"<p>Sarpi was the original name of the village located in the heart of the island. Amphitheatrically constructed on the slope of a low hill about 800 metres from Moudros Bay, the village offers stunning views to its inhabitants. Thus it was renamed &#8220;Kallithea&#8221; (good view) in 1955, as the former name was deemed Turkish. Sharpin, on the other hand, is cited in a 1361 inventory document from the Great Lavra monastery. As a result, Sharpin cannot be Turkish. Its origins are ancient, and it is one of the few Mycenaean town names that have remained on Lemnos. In particular, the term &#8220;sa-pi-de: box&#8221; appears in Mycenaean inscriptions, from which the ancient words &#8220;sarpis (the)&#8221; and &#8220;sarpos (the): ark&#8221; derived, and thus: &#8220;wooden home.&#8221; The settlement was once located further east, in the harbour of &#8220;Agios Georgios,&#8221; but residents were forced to relocate due to pirate threats on the one hand and swampy land on the other.<\\\/p>\\n<p>The &#8220;Palaiological School of Sarpi&#8221; opened in the village in 1868, the island&#8217;s first peer run school outside of the capital. With the help of the devout locals,\\u00a0the church of Agios Georgios was built from the ground up in 1868. 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Settlements\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\"},\"id\":3720,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\",\"name\":\"\\u039f\\u03b9\\u03ba\\u03b9\\u03c3\\u03bc\\u03bf\\u03af\",\"id\":\"10\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Agariones\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Agariones\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u0393\\u039a\\u0391\\u03a1\\u03a5\\u03a9\\u039d\\u0395\\u03a3_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/agariones\\\/\\\">Agariones<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/agariones\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The village of Kariones is mentioned in a codex of the Pantokratoros monastery in the year 1396, which led some to assume that it got its name from the existence of walnuts, despite the fact that walnuts do not grow in the area. The area of Laktovoidi, to the north of Agariones, is mentioned in [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8959\",\"lng\":\"25.1796\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/agariones\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The village of Kariones is mentioned in a codex of the Pantokratoros monastery in the year 1396, which led some to assume that it got its name from the existence of walnuts, despite the fact that walnuts do not grow in the area. The area of Laktovoidi, to the north of Agariones, is mentioned in [&hellip;]<\\\/p>\\n\",\"post_content\":\"The village of Kariones is mentioned in a codex of the Pantokratoros monastery in the year 1396, which led some to assume that it got its name from the existence of walnuts, despite the fact that walnuts do not grow in the area. The area of Laktovoidi, to the north of Agariones, is mentioned in a chrysobull (an imperial document granting privileges bearing a gold seal (bulla)) of 1355 as the property of the monastery of Philotheos. The site then became a Turkish tsiflik or estate that was purchased by rich Egyptians.\\r\\n\\r\\nConze paid a visit to the village in 1858, when he discovered marble fragments in an orchard\\u00a0where he sought refuge from the sun. Only the chapels of Agios Athanasios and Agios Paraskevi remain now. Agios Paraskevi features marble\\u00a0incorporated into the brickwork and an inscription stating, \\\"ESTATE OF\\u00a0ANTONIS VELISARIDI ON AUGUST 20... 192...\\\".\\u00a0 An 1858 icon by the hagiographer Efstratios Imvriou may be found within the chapel.\",\"post_title\":\"Agariones\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/agariones\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Agariones\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u0393\\u039a\\u0391\\u03a1\\u03a5\\u03a9\\u039d\\u0395\\u03a3_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.8959\",\"%_wpgmp_metabox_longitude%\":\"25.1796\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"10\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%wpcf-latitude%\":\"39.8959\",\"%wpcf-longtitude%\":\"25.1796\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses-1.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2976\",\"%_edit_lock%\":\"1658148772:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%b1%ce%b3%ce%ba%ce%b1%cf%81%cf%85%cf%8e%ce%bd%ce%b5%cf%82\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"\",\"%_wpcf-image-gallery-sort-order%\":\"22872\",\"%wpcf-code%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u0393\\u039a\\u0391\\u03a1\\u03a5\\u03a9\\u039d\\u0395\\u03a3_001.jpg, \\u0391\\u0393\\u039a\\u0391\\u03a1\\u03a5\\u03a9\\u039d\\u0395\\u03a3_001, \",\"%_et_pb_truncate_post%\":\"<p>The village of Kariones is mentioned in a codex of the Pantokratoros monastery in the year 1396, which led some to assume that it got its name from the existence of walnuts, despite the fact that walnuts do not grow in the area. The area of Laktovoidi, to the north of Agariones, is mentioned in a chrysobull (an imperial document granting privileges bearing a gold seal (bulla)) of 1355 as the property of the monastery of Philotheos. The site then became a Turkish tsiflik or estate that was purchased by rich Egyptians.<\\\/p>\\n<p>Conze paid a visit to the village in 1858, when he discovered marble fragments in an orchard\\u00a0where he sought refuge from the sun. Only the chapels of Agios Athanasios and Agios Paraskevi remain now. 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Settlements\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\"},\"id\":3721,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\",\"name\":\"\\u039f\\u03b9\\u03ba\\u03b9\\u03c3\\u03bc\\u03bf\\u03af\",\"id\":\"10\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Pedino\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Pedino\\\" width=\\\"300\\\" height=\\\"144\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u0395\\u0394\\u0399\\u039d\\u039f_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/pedino\\\/\\\">Pedino<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/pedino\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Pesperago was Pedino\\u2019s original name, and it was referenced under that name since at least the 14th century. It was renamed Pedino in 1955 because the original name was mistakenly thought to be Turkish, which it was not. After a major earthquake destroyed the village in 1968, it was abandoned by its residents who relocated [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8864\",\"lng\":\"25.1888\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/pedino\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Pesperago was Pedino\\u2019s original name, and it was referenced under that name since at least the 14th century. It was renamed Pedino in 1955 because the original name was mistakenly thought to be Turkish, which it was not. After a major earthquake destroyed the village in 1968, it was abandoned by its residents who relocated [&hellip;]<\\\/p>\\n\",\"post_content\":\"Pesperago was Pedino\\u2019s original name, and it was referenced under that name since at least the 14th century. It was renamed Pedino in 1955 because the original name was mistakenly thought to be Turkish, which it was not. After a major earthquake destroyed the village in 1968, it was abandoned by its residents who relocated to Neo Pedino, a new settlement established in a new location. In 2001, there were only\\u00a05 people living in the old village.\\r\\n\\r\\nThe settlement was initially located in Ai-Giannis, northwest of Portianos, at the foot of Ai-Lias hill, where the remnants of homes can still be seen. For unknown reasons (one typical cause for relocation was severe epidemics), the settlement was relocated to near the small salt lake that runs on from the bay of Moudros, which is now a wetland.\\r\\n\\r\\nThe village church, Agios Ioannou Prodromou, was built in 1862 in the basilica style and features a beautifully carved iconostasis. \\u00a0Palio Pedino \\u00a0(Old Pedino)has remained untouched, with \\u00a0its picturesque cobblestone streets, a cobblestone square, and stone homes with their sculpted decorative elements .\\r\\n\\r\\nThe most notable mediaeval relic in the area, Alexopyrgos or Alexiou Pyrgos, is found near Palio Pedino and was once part of the Mount Athos Pantokratoros monastery.\",\"post_title\":\"Pedino\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/pedino\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Pedino\\\" width=\\\"300\\\" height=\\\"144\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u0395\\u0394\\u0399\\u039d\\u039f_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.8864\",\"%_wpgmp_metabox_longitude%\":\"25.1888\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"10\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%wpcf-latitude%\":\"39.8864\",\"%wpcf-longtitude%\":\"25.1888\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses-1.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2979\",\"%_edit_lock%\":\"1658149133:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%80%ce%b5%ce%b4%ce%b9%ce%bd%cf%8c\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"\",\"%_wpcf-image-gallery-sort-order%\":\"22908\",\"%wpcf-code%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u0395\\u0394\\u0399\\u039d\\u039f_001.jpg, \\u03a0\\u0395\\u0394\\u0399\\u039d\\u039f_001, \",\"%_et_pb_truncate_post%\":\"<p>Pesperago was Pedino\\u2019s original name, and it was referenced under that name since at least the 14th century. It was renamed Pedino in 1955 because the original name was mistakenly thought to be Turkish, which it was not. After a major earthquake destroyed the village in 1968, it was abandoned by its residents who relocated to Neo Pedino, a new settlement established in a new location. In 2001, there were only\\u00a05 people living in the old village.<\\\/p>\\n<p>The settlement was initially located in Ai-Giannis, northwest of Portianos, at the foot of Ai-Lias hill, where the remnants of homes can still be seen. For unknown reasons (one typical cause for relocation was severe epidemics), the settlement was relocated to near the small salt lake that runs on from the bay of Moudros, which is now a wetland.<\\\/p>\\n<p>The village church, Agios Ioannou Prodromou, was built in 1862 in the basilica style and features a beautifully carved iconostasis. \\u00a0Palio Pedino \\u00a0(Old Pedino)has remained untouched, with \\u00a0its picturesque cobblestone streets, a cobblestone square, and stone homes with their sculpted decorative elements .<\\\/p>\\n<p>The most notable mediaeval relic in the area, Alexopyrgos or Alexiou Pyrgos, is found near Palio Pedino and was once part of the Mount Athos Pantokratoros monastery.<\\\/p>\\n\",\"%_et_pb_truncate_post_date%\":\"2024-02-06 03:10:08\",\"%_et_dynamic_cached_shortcodes%\":\"et_pb_section, et_pb_row, et_pb_column, et_pb_text, et_pb_sidebar, et_pb_divider, et_pb_code, et_pb_image, et_pb_social_media_follow, 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Settlements\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\"},\"id\":3723,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\",\"name\":\"\\u039f\\u03b9\\u03ba\\u03b9\\u03c3\\u03bc\\u03bf\\u03af\",\"id\":\"10\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Portianou\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Portianou\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u039f\\u03a1\\u03a4\\u0399\\u0391\\u039d\\u039f\\u03a5_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/portianou\\\/\\\">Portianou<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/portianou\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The village was originally located further west in Agios Spyridon. According to historical sources, the residents fled the settlement three centuries ago due to a cholera pandemic. The name is Latin and appears to be derived from the phrase \\u201cporto juno\\u201d, which means \\\"new port.\\\" This port was established SE of the ancient village on [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8826\",\"lng\":\"25.1757\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/portianou\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The village was originally located further west in Agios Spyridon. According to historical sources, the residents fled the settlement three centuries ago due to a cholera pandemic. The name is Latin and appears to be derived from the phrase \\u201cporto juno\\u201d, which means \\\"new port.\\\" This port was established SE of the ancient village on [&hellip;]<\\\/p>\\n\",\"post_content\":\"The village was originally located further west in Agios Spyridon. According to historical sources, the residents fled the settlement three centuries ago due to a cholera pandemic. The name is Latin and appears to be derived from the phrase \\u201cporto juno\\u201d, which means \\\"new port.\\\" This port was established SE of the ancient village on a nearby beach by the Venetians. A Venetian tower still \\u00a0marks the port that once was today.\\r\\n\\r\\nAside from agricultural and economic pursuits, the people of Portianou have developed a rich intellectual and artistic heritage that has survived to the present day. The Folklore Museum, the Graveyard of the allied soldiers stationed there in 1915 during the Gallipoli battle, the Church of the Conception of the Virgin, as well as the grand mansions\\u00a0can all be found in Portianou.\",\"post_title\":\"Portianou\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/portianou\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Portianou\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u039f\\u03a1\\u03a4\\u0399\\u0391\\u039d\\u039f\\u03a5_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.8826\",\"%_wpgmp_metabox_longitude%\":\"25.1757\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"10\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%wpcf-latitude%\":\"39.8826\",\"%wpcf-longtitude%\":\"25.1757\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses-1.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2980\",\"%_edit_lock%\":\"1658149236:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%80%ce%bf%cf%81%cf%84%ce%b9%ce%ac%ce%bd%ce%bf%cf%85\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"\",\"%_wpcf-image-gallery-sort-order%\":\"22944\",\"%wpcf-code%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u039f\\u03a1\\u03a4\\u0399\\u0391\\u039d\\u039f\\u03a5_001.jpg, \\u03a0\\u039f\\u03a1\\u03a4\\u0399\\u0391\\u039d\\u039f\\u03a5_001, \",\"%_et_pb_truncate_post%\":\"<p>The village was originally located further west in Agios Spyridon. 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The name Severgidia relates to Mount Athos, as\\u00a0chrysobulls( imperial documents granting privileges bearing a gold seal) found in the nearby estate of\\u00a0Harakas support this assumption. Because Sverdia was deemed a bad-sounding [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9502\",\"lng\":\"25.1654\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/dafni\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The original name of the village was Sverdia , which appears to be connected to the mediaeval term severgidia which means \\\"many rods\\\" (wicker). The name Severgidia relates to Mount Athos, as\\u00a0chrysobulls( imperial documents granting privileges bearing a gold seal) found in the nearby estate of\\u00a0Harakas support this assumption. 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class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/mansions\\\/\\\">Mansions<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/mansions\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Besides the grand mansions that are found in the Romeikos Gialos in Myrina, such impressive homes can be found in almost every village of the island. Built in central locations, these mansions were built by villagers of Lemnos who emigrated in the 19th century to America and Egypt. These villagers, or \\u201cEgyptians\\u201d as they were [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8774\",\"lng\":\"25.0562\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/mansions\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Besides the grand mansions that are found in the Romeikos Gialos in Myrina, such impressive homes can be found in almost every village of the island. Built in central locations, these mansions were built by villagers of Lemnos who emigrated in the 19th century to America and Egypt. These villagers, or \\u201cEgyptians\\u201d as they were [&hellip;]<\\\/p>\\n\",\"post_content\":\"Besides the grand mansions that are found in the Romeikos Gialos in Myrina, such impressive homes can be found in almost every village of the island. Built in central locations, these mansions were built by villagers of Lemnos who emigrated in the 19<sup>th<\\\/sup> century to America and Egypt. These villagers, or \\u201cEgyptians\\u201d as they were referred to, would later return and build these remarkable mansions to symbolize their economic prosperity\\r\\n\\r\\nIn contrast with the typical Lemnian home, these buildings did not have an external stairs but an impressive central entrance with stone pillars, carved stone balconies with corbels as well as other elements of decorative stone carving, which gave the facades of the buildings a monumental appearance. 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monuments\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/neoteroi_sm.png\"},\"id\":3666,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/neoteroi_sm.png\",\"name\":\"\\u039d\\u03b5\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1 \\u03bc\\u03bd\\u03b7\\u03bc\\u03b5\\u03af\\u03b1\",\"id\":\"11\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"The Gymnasium-Lyceum of Myrina, Lemnos\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"The Gymnasium-Lyceum of Myrina, Lemnos\\\" width=\\\"300\\\" height=\\\"200\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u03a4\\u0399\\u03a1\\u0399\\u039f-\\u0393\\u03a5\\u039c\\u039d\\u0391\\u03a3\\u0399\\u039f\\u03a5-\\u039b\\u03a5\\u039a\\u0395\\u0399\\u039f\\u03a5-\\u039c\\u03a5\\u03a1\\u0399\\u039d\\u0391\\u03a3_001-medium.jpg\\\" class=\\\"wp-post-image   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The exterior was decorated by engineer Michalis Michailidis's designs. The Pallimnia School Fund and Egyptian expatriates helped fund the construction. Due to seismic damage, the roof was reconstructed with wooden planks in 1981.<\\\/p>\\n\",\"location\":{\"lat\":\"39.8789\",\"lng\":\"25.0548\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-gymnasium-lyceum-of-myrina-lemnos\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The Gymnasium-Lyceum was constructed between 1925 and 1928. The exterior was decorated by engineer Michalis Michailidis's designs. The Pallimnia School Fund and Egyptian expatriates helped fund the construction. Due to seismic damage, the roof was reconstructed with wooden planks in 1981.<\\\/p>\\n\",\"post_content\":\"The Gymnasium-Lyceum was constructed between 1925 and 1928. The exterior was decorated by engineer Michalis Michailidis's designs. The Pallimnia School Fund and Egyptian expatriates helped fund the construction. Due to seismic damage, the roof was reconstructed with wooden planks in 1981.\",\"post_title\":\"The Gymnasium-Lyceum of Myrina, Lemnos\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-gymnasium-lyceum-of-myrina-lemnos\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"The Gymnasium-Lyceum of Myrina, Lemnos\\\" width=\\\"300\\\" height=\\\"200\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u03a4\\u0399\\u03a1\\u0399\\u039f-\\u0393\\u03a5\\u039c\\u039d\\u0391\\u03a3\\u0399\\u039f\\u03a5-\\u039b\\u03a5\\u039a\\u0395\\u0399\\u039f\\u03a5-\\u039c\\u03a5\\u03a1\\u0399\\u039d\\u0391\\u03a3_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"11\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.8789\",\"%_wpgmp_metabox_longitude%\":\"25.0548\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2892\",\"%_edit_lock%\":\"1657803837:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%ba%cf%84%ce%af%cf%81%ce%b9%ce%bf-%ce%b3%cf%85%ce%bc%ce%bd%ce%b1%cf%83%ce%af%ce%bf%cf%85-%ce%bb%cf%85%ce%ba%ce%b5%ce%af%ce%bf%cf%85-%cf%83%cf%84%ce%b7-%ce%bc%cf%8d%cf%81%ce%b9%ce%bd%ce%b1-%ce%bb\",\"%wpcf-latitude%\":\"\",\"%wpcf-longtitude%\":\"\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u03a4\\u0399\\u03a1\\u0399\\u039f-\\u0393\\u03a5\\u039c\\u039d\\u0391\\u03a3\\u0399\\u039f\\u03a5-\\u039b\\u03a5\\u039a\\u0395\\u0399\\u039f\\u03a5-\\u039c\\u03a5\\u03a1\\u0399\\u039d\\u0391\\u03a3_001.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"21640\",\"%wpcf-code%\":\"\",\"%wpcf-mapicon%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u03a4\\u0399\\u03a1\\u0399\\u039f-\\u0393\\u03a5\\u039c\\u039d\\u0391\\u03a3\\u0399\\u039f\\u03a5-\\u039b\\u03a5\\u039a\\u0395\\u0399\\u039f\\u03a5-\\u039c\\u03a5\\u03a1\\u0399\\u039d\\u0391\\u03a3_001.jpg, \\u039a\\u03a4\\u0399\\u03a1\\u0399\\u039f \\u0393\\u03a5\\u039c\\u039d\\u0391\\u03a3\\u0399\\u039f\\u03a5-\\u039b\\u03a5\\u039a\\u0395\\u0399\\u039f\\u03a5 \\u039c\\u03a5\\u03a1\\u0399\\u039d\\u0391\\u03a3_001, \",\"%_et_pb_truncate_post%\":\"<p>The Gymnasium-Lyceum was constructed between 1925 and 1928. The exterior was decorated by engineer Michalis Michailidis&#8217;s designs. The Pallimnia School Fund and Egyptian expatriates helped fund the construction. Due to seismic damage, the roof was reconstructed with wooden planks in 1981.<\\\/p>\\n\",\"%_et_pb_truncate_post_date%\":\"2023-01-03 14:57:29\",\"taxonomy=point_category\":\"Modern monuments\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/neoteroi_sm.png\"},\"id\":3668,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/neoteroi_sm.png\",\"name\":\"\\u039d\\u03b5\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1 \\u03bc\\u03bd\\u03b7\\u03bc\\u03b5\\u03af\\u03b1\",\"id\":\"11\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Agia Paraskevi, Vondela\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Agia Paraskevi, Vondela\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u0393\\u0399\\u0391-\\u03a0\\u0391\\u03a1\\u0391\\u03a3\\u039a\\u0395\\u03a5\\u0397-\\u0392\\u039f\\u039d\\u03a4\\u0395\\u039b\\u0391_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/agia-paraskevi-vondela\\\/\\\">Agia Paraskevi, Vondela<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/agia-paraskevi-vondela\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The small chapel at the base of the Castle of Myrina is dedicated to Agia Paraskevi. It is situated close to the Vontela mansion which acts as the outer limit for the town of Myrina to the Castle\\u2019s\\u00a0peninsula, and is commonly referred\\u00a0to as \\\"Agia Paraskevi Vondela.\\\" The little church, usually whitewashed a bright white, adds [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8775\",\"lng\":\"25.0582\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/agia-paraskevi-vondela\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The small chapel at the base of the Castle of Myrina is dedicated to Agia Paraskevi. It is situated close to the Vontela mansion which acts as the outer limit for the town of Myrina to the Castle\\u2019s\\u00a0peninsula, and is commonly referred\\u00a0to as \\\"Agia Paraskevi Vondela.\\\" The little church, usually whitewashed a bright white, adds [&hellip;]<\\\/p>\\n\",\"post_content\":\"The small chapel at the base of the Castle of Myrina is dedicated to Agia Paraskevi.\\r\\n\\r\\nIt is situated close to the Vontela mansion which acts as the outer limit for the town of Myrina to the Castle\\u2019s\\u00a0peninsula, and is commonly referred\\u00a0to as \\\"Agia Paraskevi Vondela.\\\"\\r\\n\\r\\nThe little church, usually whitewashed a bright white, adds its own color to this old Lemnos location.\",\"post_title\":\"Agia Paraskevi, Vondela\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/agia-paraskevi-vondela\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Agia Paraskevi, Vondela\\\" width=\\\"300\\\" 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fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/myrina\\\/\\\">Myrina<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/myrina\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The capital of Lemnos is Myrina. Antiquities discovered in the city of Myrina show that it was inhabited before the Bronze Age. It was named after Myrina, daughter of Iolkos, \\u00a0Krithea's ruler and spouse of Thoanta, the first mythological king of Lemnos. Its foundation dates back to\\u00a0the 12th or 13th century BC, when Lemnos was [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8789\",\"lng\":\"25.0548\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/myrina\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The capital of Lemnos is Myrina. Antiquities discovered in the city of Myrina show that it was inhabited before the Bronze Age. It was named after Myrina, daughter of Iolkos, \\u00a0Krithea's ruler and spouse of Thoanta, the first mythological king of Lemnos. Its foundation dates back to\\u00a0the 12th or 13th century BC, when Lemnos was [&hellip;]<\\\/p>\\n\",\"post_content\":\"The capital of Lemnos is Myrina. Antiquities discovered in the city of Myrina show that it was inhabited before the Bronze Age. It was named after Myrina, daughter of Iolkos, \\u00a0Krithea's ruler and spouse of Thoanta, the first mythological king of Lemnos. Its foundation dates back to\\u00a0the 12th or 13th century BC, when Lemnos was governed by the Minyae, and the first fortress was most likely completed at that time. It was the strongest citadel on Lemnos at all periods for this reason, and the city was known as a Castle\\u00a0from the late Byzantine period until 1955.\\r\\n\\r\\nThe scenic streets, the stately homes in the Romeikos Gialos, the market, and the harbour all have an authentic and traditional character. The Venetian Castle with its roaming\\u00a0deer, the Archaeological Museum, the prehistoric city, the Metropolitan Church of the Holy Trinity, the Ecclesiastical Museum, and Dapia atop the hill of Tsas are all noteworthy attractions. The closest beaches are Romeikos\\u00a0Gialos and Riha Nera, both of which are accessible on foot. The beach of Avlonas\\u00a0is located just outside of Myrina on the way to Kaspakas. The hotel Porto Myrina, with the ancient temple of the Goddess Artemis situated in its courtyard, dominates the left side of the city.\",\"post_title\":\"Myrina\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/myrina\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Myrina\\\" width=\\\"300\\\" height=\\\"169\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039c\\u03a5\\u03a1\\u0399\\u039d\\u0391_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"10\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.8789\",\"%_wpgmp_metabox_longitude%\":\"25.0548\",\"%wpcf-latitude%\":\"39.8789\",\"%wpcf-longtitude%\":\"25.0548\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses-1.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2907\",\"%_edit_lock%\":\"1658298702:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%bc%cf%8d%cf%81%ce%b9%ce%bd%ce%b1\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039c\\u03a5\\u03a1\\u0399\\u039d\\u0391_001.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"23016\",\"%wpcf-code%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039c\\u03a5\\u03a1\\u0399\\u039d\\u0391_001.jpg, \\u039c\\u03a5\\u03a1\\u0399\\u039d\\u0391_001, \",\"%_et_pb_truncate_post%\":\"<p>The capital of Lemnos is Myrina. Antiquities discovered in the city of Myrina show that it was inhabited before the Bronze Age. It was named after Myrina, daughter of Iolkos, \\u00a0Krithea&#8217;s ruler and spouse of Thoanta, the first mythological king of Lemnos. Its foundation dates back to\\u00a0the 12th or 13th century BC, when Lemnos was governed by the Minyae, and the first fortress was most likely completed at that time. It was the strongest citadel on Lemnos at all periods for this reason, and the city was known as a Castle\\u00a0from the late Byzantine period until 1955.<\\\/p>\\n<p>The scenic streets, the stately homes in the Romeikos Gialos, the market, and the harbour all have an authentic and traditional character. The Venetian Castle with its roaming\\u00a0deer, the Archaeological Museum, the prehistoric city, the Metropolitan Church of the Holy Trinity, the Ecclesiastical Museum, and Dapia atop the hill of Tsas are all noteworthy attractions. 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Settlements\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\"},\"id\":3726,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\",\"name\":\"\\u039f\\u03b9\\u03ba\\u03b9\\u03c3\\u03bc\\u03bf\\u03af\",\"id\":\"10\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Kontias\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Kontias\\\" width=\\\"300\\\" height=\\\"199\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u039f\\u039d\\u03a4\\u0399\\u0391\\u03a3_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kontias\\\/\\\">Kontias<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kontias\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>In 1918, the settlement was initially established as a community under the name Kondias, which was later changed to Kontias in 1940, named after Kontea, a Byzantine landowner in the region. According to oral tradition, the settlement was originally near the sea, but was abandoned due to pirate raids. It is possible that the former [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8633\",\"lng\":\"25.1482\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kontias\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>In 1918, the settlement was initially established as a community under the name Kondias, which was later changed to Kontias in 1940, named after Kontea, a Byzantine landowner in the region. According to oral tradition, the settlement was originally near the sea, but was abandoned due to pirate raids. It is possible that the former [&hellip;]<\\\/p>\\n\",\"post_content\":\"In 1918, the settlement was initially established as a community under the name Kondias, which was later changed to Kontias in 1940, named after Kontea, a Byzantine landowner in the region. According to oral tradition, the settlement was originally near the sea, but was abandoned due to pirate raids. It is possible that the former location corresponds to Nevgati, which had a temple and a few residents. However, the most likely location is the port of Agios Giannis on the harbour of Kontias, where a wrecked fortress still stands. The earliest\\u00a0account of the settlement in its current position is from 1785.\\r\\n\\r\\nAgios Ioannis Prodromos is the village's oldest church. Despite its small size,\\u00a0 it is \\u00a0built like a fortress, complete with battlements\\u00a0and cannons. It is thought to have been constructed in the 16th century. The church has historic icons and served as a museum in the 1970s.\\r\\n\\r\\nThe parish church of Agios Dimitrios, built in the basilica style with a covered exonarthex and monolithic columns with decorative capitals, was consecrated in 1867. It is an impressive church with its \\u00a0large stone bell tower that was added later on.\\u00a0In 1938, the Nativity of Christ Church, which had originally belonged to the Lavra, was burned down and rebuilt.\",\"post_title\":\"Kontias\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kontias\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Kontias\\\" width=\\\"300\\\" height=\\\"199\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u039f\\u039d\\u03a4\\u0399\\u0391\\u03a3_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"10\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.8633\",\"%_wpgmp_metabox_longitude%\":\"25.1482\",\"%wpcf-latitude%\":\"39.8633\",\"%wpcf-longtitude%\":\"25.1482\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses-1.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2914\",\"%_edit_lock%\":\"1658298798:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%ba%ce%bf%ce%bd%cf%84%ce%b9%ce%ac%cf%82\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u039f\\u039d\\u03a4\\u0399\\u0391\\u03a3_001.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"23054, 23055\",\"%wpcf-code%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u039f\\u039d\\u03a4\\u0399\\u0391\\u03a3_002.jpg, \\u039a\\u039f\\u039d\\u03a4\\u0399\\u0391\\u03a3_002, \",\"%_et_pb_truncate_post%\":\"<p>In 1918, the settlement was initially established as a community under the name Kondias, which was later changed to Kontias in 1940, named after Kontea, a Byzantine landowner in the region. According to oral tradition, the settlement was originally near the sea, but was abandoned due to pirate raids. It is possible that the former location corresponds to Nevgati, which had a temple and a few residents. However, the most likely location is the port of Agios Giannis on the harbour of Kontias, where a wrecked fortress still stands. The earliest\\u00a0account of the settlement in its current position is from 1785.<\\\/p>\\n<p>Agios Ioannis Prodromos is the village&#8217;s oldest church. Despite its small size,\\u00a0 it is \\u00a0built like a fortress, complete with battlements\\u00a0and cannons. It is thought to have been constructed in the 16th century. The church has historic icons and served as a museum in the 1970s.<\\\/p>\\n<p>The parish church of Agios Dimitrios, built in the basilica style with a covered exonarthex and monolithic columns with decorative capitals, was consecrated in 1867. 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Settlements\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\"},\"id\":3727,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\",\"name\":\"\\u039f\\u03b9\\u03ba\\u03b9\\u03c3\\u03bc\\u03bf\\u03af\",\"id\":\"10\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Repanidi\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Repanidi\\\" width=\\\"300\\\" height=\\\"199\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a1\\u0395\\u03a0\\u0391\\u039d\\u0399\\u0394\\u0399_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/repanidi\\\/\\\">Repanidi<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/repanidi\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>In 1285, monastery papers mention the village by its current name for the first time. The terms Repanidion or Rapanidi appear in community papers from the 13th to the 16th centuries, and they appear again in the 19th century in the forms Repanidion, Rapanidi, Ropanidi, Repanidi, or Repanidi. As a result, the village's name is [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9221\",\"lng\":\"25.2965\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/repanidi\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>In 1285, monastery papers mention the village by its current name for the first time. The terms Repanidion or Rapanidi appear in community papers from the 13th to the 16th centuries, and they appear again in the 19th century in the forms Repanidion, Rapanidi, Ropanidi, Repanidi, or Repanidi. As a result, the village's name is [&hellip;]<\\\/p>\\n\",\"post_content\":\"In 1285, monastery papers mention the village by its current name for the first time. The terms Repanidion or Rapanidi appear in community papers from the 13th to the 16th centuries, and they appear again in the 19th century in the forms Repanidion, Rapanidi, Ropanidi, Repanidi, or Repanidi. As a result, the village's name is most likely derived from the wild radish. The earliest occupants of Repanidi came from Iphaistia which had begun to be abandoned by its population around\\u00a0the 2nd century.\\r\\n\\r\\nAthanasios, the new martyr, was born in Repanidi, which was conquered by the Turks in 1846 and he was sent to Constantinople by ship. The martyr, however, was never to reach the city since the guards chained him, then\\u00a0tossed him\\u00a0into the water and drowned him while sailing in the Hellespont, knowing that he would most likely be exonerated in the higher court because he had done no crime.\\r\\n\\r\\nThe importance of the Repanidi area has been recognised since ancient times, when the famous \\\"Limnia Earth\\\" was mined in the nearby region of Agiochoma.\",\"post_title\":\"Repanidi\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/repanidi\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Repanidi\\\" width=\\\"300\\\" height=\\\"199\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a1\\u0395\\u03a0\\u0391\\u039d\\u0399\\u0394\\u0399_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"10\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.9221\",\"%_wpgmp_metabox_longitude%\":\"25.2965\",\"%wpcf-latitude%\":\"39.9221\",\"%wpcf-longtitude%\":\"25.2965\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses-1.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2900\",\"%_edit_lock%\":\"1658298743:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%81%ce%b5%cf%80%ce%b1%ce%bd%ce%af%ce%b4%ce%b9\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a1\\u0395\\u03a0\\u0391\\u039d\\u0399\\u0394\\u0399_001.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"23092, 23093\",\"%wpcf-code%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a1\\u0395\\u03a0\\u0391\\u039d\\u0399\\u0394\\u0399_002.jpg, \\u03a1\\u0395\\u03a0\\u0391\\u039d\\u0399\\u0394\\u0399_002, \",\"%_et_pb_truncate_post%\":\"<p>In 1285, monastery papers mention the village by its current name for the first time. The terms Repanidion or Rapanidi appear in community papers from the 13th to the 16th centuries, and they appear again in the 19th century in the forms Repanidion, Rapanidi, Ropanidi, Repanidi, or Repanidi. As a result, the village&#8217;s name is most likely derived from the wild radish. The earliest occupants of Repanidi came from Iphaistia which had begun to be abandoned by its population around\\u00a0the 2nd century.<\\\/p>\\n<p>Athanasios, the new martyr, was born in Repanidi, which was conquered by the Turks in 1846 and he was sent to Constantinople by ship. 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Settlements\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\"},\"id\":3729,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\",\"name\":\"\\u039f\\u03b9\\u03ba\\u03b9\\u03c3\\u03bc\\u03bf\\u03af\",\"id\":\"10\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Kotsinas\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Kotsinas\\\" width=\\\"300\\\" height=\\\"185\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u039f\\u03a4\\u03a3\\u0399\\u039d\\u0391\\u03a3_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kotsinas\\\/\\\">Kotsinas<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kotsinas\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The name of this village was derived from the red colour of the soil in the area, particularly the famed Lemnian earth, which was mined from the nearby Despotis hill, the ancients' Mosychlos, near the Savior's chapel. In 1981, it was designated as a distinct village inside the Repanidi community, known as Kotsinas. The village\\u00a0was [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9408\",\"lng\":\"25.2811\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kotsinas\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The name of this village was derived from the red colour of the soil in the area, particularly the famed Lemnian earth, which was mined from the nearby Despotis hill, the ancients' Mosychlos, near the Savior's chapel. In 1981, it was designated as a distinct village inside the Repanidi community, known as Kotsinas. The village\\u00a0was [&hellip;]<\\\/p>\\n\",\"post_content\":\"The name of this village was derived from the red colour of the soil in the area, particularly the famed Lemnian earth, which was mined from the nearby Despotis hill, the ancients' Mosychlos, near the Savior's chapel. In 1981, it was designated as a distinct village inside the Repanidi community, known as Kotsinas.\\r\\n\\r\\nThe village\\u00a0was a major harbour throughout the Middle Ages. It was originally a\\u00a0port of the ancient town of Iphaistia, but in 1361 it was given an imposing Castle. The church of Zoodochos Pigi is built atop an underground well, \\\"agiasma,\\\" on the hill of Kotsinos, inside the castle. The well source is reached by a descending 64 steps (previously with 57 or 51) to almost sea level. The underground passage was apparently dug when the artificial hill of the castle was completed, so that the water necessary for sieges would not be wasted. The present holy water was created in 1918, and the new church was established in 1954 with the help of expatriates from the United States and Australia. Only one entablature from the Byzantine era has survived.\\r\\n\\r\\nPottery has a long history in the Kotsina area, dating back to the Middle Ages, if not earlier.\\r\\n\\r\\nAgios Ypatios, sometimes known as Anypatis, is a small town near Repanidi. Anypatis was quite mobile during the late Turkish period (1650-1912). Repanidi was most likely initially close by.\",\"post_title\":\"Kotsinas\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kotsinas\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Kotsinas\\\" width=\\\"300\\\" height=\\\"185\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u039f\\u03a4\\u03a3\\u0399\\u039d\\u0391\\u03a3_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"10\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.9408\",\"%_wpgmp_metabox_longitude%\":\"25.2811\",\"%wpcf-latitude%\":\"39.9408\",\"%wpcf-longtitude%\":\"25.2811\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses-1.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2911\",\"%_edit_lock%\":\"1658298974:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%ba%cf%8c%cf%84%cf%83%ce%b9%ce%bd%ce%b1%cf%82\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u039f\\u03a4\\u03a3\\u0399\\u039d\\u0391\\u03a3_001.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"23129\",\"%wpcf-code%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u039f\\u03a4\\u03a3\\u0399\\u039d\\u0391\\u03a3_001.jpg, \\u039a\\u039f\\u03a4\\u03a3\\u0399\\u039d\\u0391\\u03a3_001, \",\"%_et_pb_truncate_post%\":\"<p>The name of this village was derived from the red colour of the soil in the area, particularly the famed Lemnian earth, which was mined from the nearby Despotis hill, the ancients&#8217; Mosychlos, near the Savior&#8217;s chapel. In 1981, it was designated as a distinct village inside the Repanidi community, known as Kotsinas.<\\\/p>\\n<p>The village\\u00a0was a major harbour throughout the Middle Ages. It was originally a\\u00a0port of the ancient town of Iphaistia, but in 1361 it was given an imposing Castle. The church of Zoodochos Pigi is built atop an underground well, &#8220;agiasma,&#8221; on the hill of Kotsinos, inside the castle. The well source is reached by a descending 64 steps (previously with 57 or 51) to almost sea level. The underground passage was apparently dug when the artificial hill of the castle was completed, so that the water necessary for sieges would not be wasted. The present holy water was created in 1918, and the new church was established in 1954 with the help of expatriates from the United States and Australia. Only one entablature from the Byzantine era has survived.<\\\/p>\\n<p>Pottery has a long history in the Kotsina area, dating back to the Middle Ages, if not earlier.<\\\/p>\\n<p>Agios Ypatios, sometimes known as Anypatis, is a small town near Repanidi. Anypatis was quite mobile during the late Turkish period (1650-1912). 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class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kontopouli\\\/\\\">Kontopouli<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kontopouli\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The Byzantine landowner Kontopoulos gave this settlement its name. 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class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kalliopi\\\/\\\">Kalliopi<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kalliopi\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The settlement was founded in 1200, when the era of decline had\\u00a0 begun for Iphaistia. At the time, the village's founder was the wealthy Kalliopi or Kalli, who had a farm in the region, having migrated from Iphaistia.\\u00a0 According to one story, \\u00a0Kalliopi had been exiled from Iphaistia for her impure conduct. A marble sarcophagus [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9200\",\"lng\":\"25.3371\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kalliopi\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The settlement was founded in 1200, when the era of decline had\\u00a0 begun for Iphaistia. At the time, the village's founder was the wealthy Kalliopi or Kalli, who had a farm in the region, having migrated from Iphaistia.\\u00a0 According to one story, \\u00a0Kalliopi had been exiled from Iphaistia for her impure conduct. A marble sarcophagus [&hellip;]<\\\/p>\\n\",\"post_content\":\"The settlement was founded in 1200, when the era of decline had\\u00a0 begun for Iphaistia. 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It is protected against environmental conditions as part of the NATURA network.\\r\\n\\r\\nThe Early Christian tomb in the cemetery of St. Annas may also be visited in the village.\",\"post_title\":\"Kalliopi\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kalliopi\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Kalliopi\\\" width=\\\"300\\\" height=\\\"150\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u0391\\u039b\\u039b\\u0399\\u039f\\u03a0\\u0397_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"10\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.9200\",\"%_wpgmp_metabox_longitude%\":\"25.3371\",\"%wpcf-latitude%\":\"39.9200\",\"%wpcf-longtitude%\":\"25.3371\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses-1.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2922\",\"%_edit_lock%\":\"1658299230:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%ba%ce%b1%ce%bb%ce%bb%ce%b9%cf%8c%cf%80%ce%b7\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u0391\\u039b\\u039b\\u0399\\u039f\\u03a0\\u0397_001.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"23201\",\"%wpcf-code%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u0391\\u039b\\u039b\\u0399\\u039f\\u03a0\\u0397_001.jpg, \\u039a\\u0391\\u039b\\u039b\\u0399\\u039f\\u03a0\\u0397_001, \",\"%_et_pb_truncate_post%\":\"<p>The settlement was founded in 1200, when the era of decline had\\u00a0 begun for Iphaistia. At the time, the village&#8217;s founder was the wealthy Kalliopi or Kalli, who had a farm in the region, having migrated from Iphaistia.\\u00a0 According to one story, \\u00a0Kalliopi had been exiled from Iphaistia for her impure conduct. A marble sarcophagus with an etched cross and the statement &#8220;Here lays the servant of God Kalli&#8221; is kept in the local cemetery.<\\\/p>\\n<p>Named after its horn-like shape, Keros Bay serves as the village beach. The bay is nearly three kilometres long and was a major harbour until the late Middle Ages.<\\\/p>\\n<p>Agios Georgios is the village&#8217;s patron saint, and a basilica-style church without a dome was constructed in his honour in 1869. Every year on St. George&#8217;s Day, traditional horse races are held in his honor. This tradition dates to the\\u00a0mid-nineteenth century.<\\\/p>\\n<p>Hortarolimni, one of the most significant wetlands in the prefecture of Lemnos, is located near the settlement. 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Settlements\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\"},\"id\":3732,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\",\"name\":\"\\u039f\\u03b9\\u03ba\\u03b9\\u03c3\\u03bc\\u03bf\\u03af\",\"id\":\"10\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Plaka\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Plaka\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/plaka-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/plaka\\\/\\\">Plaka<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/plaka\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Residents of St. Ypatios and Iphaistia who owned agriculture land in the area used to visit Plaka on a seasonal basis. After 1823, a few people began to settle there permanently, and by 1860, a large group had assembled to form a community. Simferoupolis was the village's original name which was given by the archbishop [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"40.0039\",\"lng\":\"25.4233\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/plaka\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Residents of St. Ypatios and Iphaistia who owned agriculture land in the area used to visit Plaka on a seasonal basis. After 1823, a few people began to settle there permanently, and by 1860, a large group had assembled to form a community. Simferoupolis was the village's original name which was given by the archbishop [&hellip;]<\\\/p>\\n\",\"post_content\":\"Residents of St. Ypatios and Iphaistia who owned agriculture land in the area used to visit Plaka on a seasonal basis. After 1823, a few people began to settle there permanently, and by 1860, a large group had assembled to form a community. Simferoupolis was the village's original name which was given by the archbishop of Lemnos, Joachim III whom the people of Agios Ypatios approached with their decision to form a new community. They had been obliged to leave Agios Ypatios for reasons of interest. The new name of the settlement came from the Plaka cape, which has impressive grey and black horizontal rocks.\\u00a0 Because the cape is situated in the centre of the straight line connecting Troas and Mount Athos, some believe it was the ancients' \\\" Ermaion Lepas,\\\" through which the news of Troy's fall was conveyed by fire.\\r\\n\\r\\nThe presence of a fortified settlement in the Plaka region has been documented since\\u00a01355. It is most likely linked to the \\\"Castle of the Kastriots,\\\" where Kritovoulos landed from Imvros in 1459 and forced the Venetians off the island.\\r\\n\\r\\nThe remnants of an old sunken city were discovered in the southern portion of the Vriokastro peninsula, roughly 800 metres from the coast and east of the Vina reef. Another sunken ancient city has been discovered off the east coast of Greece in the Mythones sea region. Linking them to the Homeric islet of Chrysi, which sunk in 197 BC, Choiseul-Guffier was the first to refer to the ruins in 1785.\",\"post_title\":\"Plaka\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/plaka\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Plaka\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/plaka-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"40.0039\",\"%_wpgmp_metabox_longitude%\":\"25.4233\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"10\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%wpcf-latitude%\":\"40.0039\",\"%wpcf-longtitude%\":\"25.4233\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses-1.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2986\",\"%_edit_lock%\":\"1658299269:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%80%ce%bb%ce%ac%ce%ba%ce%b1\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"\",\"%_wpcf-image-gallery-sort-order%\":\"23237\",\"%wpcf-code%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/plaka.jpg, plaka, \",\"%_et_pb_truncate_post%\":\"<p>Residents of St. Ypatios and Iphaistia who owned agriculture land in the area used to visit Plaka on a seasonal basis. After 1823, a few people began to settle there permanently, and by 1860, a large group had assembled to form a community. Simferoupolis was the village&#8217;s original name which was given by the archbishop of Lemnos, Joachim III whom the people of Agios Ypatios approached with their decision to form a new community. They had been obliged to leave Agios Ypatios for reasons of interest. The new name of the settlement came from the Plaka cape, which has impressive grey and black horizontal rocks.\\u00a0 Because the cape is situated in the centre of the straight line connecting Troas and Mount Athos, some believe it was the ancients&#8217; &#8221; Ermaion Lepas,&#8221; through which the news of Troy&#8217;s fall was conveyed by fire.<\\\/p>\\n<p>The presence of a fortified settlement in the Plaka region has been documented since\\u00a01355. It is most likely linked to the &#8220;Castle of the Kastriots,&#8221; where Kritovoulos landed from Imvros in 1459 and forced the Venetians off the island.<\\\/p>\\n<p>The remnants of an old sunken city were discovered in the southern portion of the Vriokastro peninsula, roughly 800 metres from the coast and east of the Vina reef. Another sunken ancient city has been discovered off the east coast of Greece in the Mythones sea region. 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Settlements\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\"},\"id\":3734,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\",\"name\":\"\\u039f\\u03b9\\u03ba\\u03b9\\u03c3\\u03bc\\u03bf\\u03af\",\"id\":\"10\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Panagia\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Panagia\\\" width=\\\"300\\\" height=\\\"150\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u0391\\u039d\\u0391\\u0393\\u0399\\u0391_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/panagia\\\/\\\">Panagia<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/panagia\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>According to local folklore, the area name of Panagia pre-existed the village name, and it came from some old monastery. There was no village in the area of NE Lemnos between the town of Kontopouli and the Plaka cape until the middle of the 19th century. Only a few scattered estate cottages belonging to the [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9815\",\"lng\":\"25.4022\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/panagia\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>According to local folklore, the area name of Panagia pre-existed the village name, and it came from some old monastery. There was no village in the area of NE Lemnos between the town of Kontopouli and the Plaka cape until the middle of the 19th century. Only a few scattered estate cottages belonging to the [&hellip;]<\\\/p>\\n\",\"post_content\":\"According to local folklore, the area name of Panagia pre-existed the village name, and it came from some old monastery. 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The area \\\"Panagia\\\" \\u00a0was chosen, where the old Byzantine monastery was built at the foot of the\\\"Alepotrypes\\u201d hill, most likely because it was almost equal distance from the western and eastern coastlines, thus providing more protection.\",\"post_title\":\"Panagia\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/panagia\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Panagia\\\" width=\\\"300\\\" height=\\\"150\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u0391\\u039d\\u0391\\u0393\\u0399\\u0391_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"10\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.9815\",\"%_wpgmp_metabox_longitude%\":\"25.4022\",\"%wpcf-latitude%\":\"39.9815\",\"%wpcf-longtitude%\":\"25.4022\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses-1.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2904\",\"%_edit_lock%\":\"1658299345:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%80%ce%b1%ce%bd%ce%b1%ce%b3%ce%b9%ce%ac\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u0391\\u039d\\u0391\\u0393\\u0399\\u0391_001.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"23273\",\"%wpcf-code%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u0391\\u039d\\u0391\\u0393\\u0399\\u0391_001.jpg, \\u03a0\\u0391\\u039d\\u0391\\u0393\\u0399\\u0391_001, \",\"%_et_pb_truncate_post%\":\"<p>According to local folklore, the area name of Panagia pre-existed the village name, and it came from some old monastery. 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Settlements\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\"},\"id\":3736,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\",\"name\":\"\\u039f\\u03b9\\u03ba\\u03b9\\u03c3\\u03bc\\u03bf\\u03af\",\"id\":\"10\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Moudros\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Moudros\\\" width=\\\"300\\\" height=\\\"150\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039c\\u039f\\u03a5\\u0394\\u03a1\\u039f\\u03a3_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/moudros\\\/\\\">Moudros<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/moudros\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Human occupation in the Moudros area dates back to prehistoric times. The origin of the names Moudron\\u00a0and Moudros\\u00a0is uncertain. It is more likely that it formed as a result of a \\\"mydro,\\\" a granite rock formed by solidified lava that existed near the harbour and to which the sailors anchored their ships. The Taxiarches' church [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8746\",\"lng\":\"25.2675\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/moudros\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Human occupation in the Moudros area dates back to prehistoric times. The origin of the names Moudron\\u00a0and Moudros\\u00a0is uncertain. It is more likely that it formed as a result of a \\\"mydro,\\\" a granite rock formed by solidified lava that existed near the harbour and to which the sailors anchored their ships. The Taxiarches' church [&hellip;]<\\\/p>\\n\",\"post_content\":\"Human occupation in the Moudros area dates back to prehistoric times. The origin of the names Moudron\\u00a0and Moudros\\u00a0is uncertain. It is more likely that it formed as a result of a \\\"mydro,\\\" a granite rock formed by solidified lava that existed near the harbour and to which the sailors anchored their ships.\\r\\n\\r\\nThe Taxiarches' church was built \\\"BY THE LOCALS OF MOUDROS\\\" in 1835. It features three aisles and a exonarthex (added later), and its wooden iconostasis is claimed to be a duplicate of a Smyrna church\\u2019s iconostasis. The monumental church of Evangelistria was built in 1903-04. It is a three-aisled basilica with magnificent architectural characteristics, including a bell tower. Admiral Koundouriotis gave\\u00a0the epitaph as a gift. The\\u00a0Agia Marina parish of the Koutloumousiou monastery used to be in the region where the church was built,\\u00a0the\\u00a0altar and several structures are preserved to this day and can be viewed. The parish\\u00a0ended in tragedy. When they discovered five Turkish officers dead in a well of the estate, the Turks burnt it down along with seven monks. Only two monks escaped, and they sought safety in Koutloumousi, where they claimed that the Turks were killed by\\u00a0residents in order to incriminate the monks, dissolve the estate and seize its lands. The abbot then imposed a fine\\u00a0on the village, which has just recently been paid off.\",\"post_title\":\"Moudros\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/moudros\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Moudros\\\" width=\\\"300\\\" height=\\\"150\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039c\\u039f\\u03a5\\u0394\\u03a1\\u039f\\u03a3_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"10\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.8746\",\"%_wpgmp_metabox_longitude%\":\"25.2675\",\"%wpcf-latitude%\":\"39.8746\",\"%wpcf-longtitude%\":\"25.2675\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses-1.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2908\",\"%_edit_lock%\":\"1658299437:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%bc%ce%bf%cf%8d%ce%b4%cf%81%ce%bf%cf%82\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039c\\u039f\\u03a5\\u0394\\u03a1\\u039f\\u03a3_001.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"23309\",\"%wpcf-code%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039c\\u039f\\u03a5\\u0394\\u03a1\\u039f\\u03a3_001.jpg, \\u039c\\u039f\\u03a5\\u0394\\u03a1\\u039f\\u03a3_001, \",\"%_et_pb_truncate_post%\":\"<p>Human occupation in the Moudros area dates back to prehistoric times. The origin of the names Moudron\\u00a0and Moudros\\u00a0is uncertain. It is more likely that it formed as a result of a &#8220;mydro,&#8221; a granite rock formed by solidified lava that existed near the harbour and to which the sailors anchored their ships.<\\\/p>\\n<p>The Taxiarches&#8217; church was built &#8220;BY THE LOCALS OF MOUDROS&#8221; in 1835. It features three aisles and a exonarthex (added later), and its wooden iconostasis is claimed to be a duplicate of a Smyrna church\\u2019s iconostasis. The monumental church of Evangelistria was built in 1903-04. It is a three-aisled basilica with magnificent architectural characteristics, including a bell tower. Admiral Koundouriotis gave\\u00a0the epitaph as a gift. The\\u00a0Agia Marina parish of the Koutloumousiou monastery used to be in the region where the church was built,\\u00a0the\\u00a0altar and several structures are preserved to this day and can be viewed. The parish\\u00a0ended in tragedy. 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fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/romanou\\\/\\\">Romanou<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/romanou\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Despite the lack of documentation, the name most likely comes from an old landowner named \\\"Romanos,\\\" as was the custom then. In 1918 however, the settlement was renamed Romanos and became a community. It was renamed Romanon\\u00a0in 1940, but it is once again Romanou. The current inhabitants settled there around 200 years ago to defend [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9054\",\"lng\":\"25.2874\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/romanou\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Despite the lack of documentation, the name most likely comes from an old landowner named \\\"Romanos,\\\" as was the custom then. In 1918 however, the settlement was renamed Romanos and became a community. It was renamed Romanon\\u00a0in 1940, but it is once again Romanou. The current inhabitants settled there around 200 years ago to defend [&hellip;]<\\\/p>\\n\",\"post_content\":\"Despite the lack of documentation, the name most likely comes from an old landowner named \\\"Romanos,\\\" as was the custom then. 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  <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/roussopouli\\\/\\\">Roussopouli<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/roussopouli\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The Byzantine landowner Rossopoulos or Roussopoulos is credited for the village's name. According to tradition, the village was originally built northeast of today's site, along the sea towards Hortarolimni, but the residents abandoned it due to pirate threats and relocated it behind the hill of Korakas. Old temple ruins may be found in numerous locations [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8827\",\"lng\":\"25.3083\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/roussopouli\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The Byzantine landowner Rossopoulos or Roussopoulos is credited for the village's name. According to tradition, the village was originally built northeast of today's site, along the sea towards Hortarolimni, but the residents abandoned it due to pirate threats and relocated it behind the hill of Korakas. Old temple ruins may be found in numerous locations [&hellip;]<\\\/p>\\n\",\"post_content\":\"The Byzantine landowner Rossopoulos or Roussopoulos is credited for the village's name. According to tradition, the village was originally built northeast of today's site, along the sea towards Hortarolimni, but the residents abandoned it due to pirate threats and relocated it behind the hill of Korakas. Old temple ruins may be found in numerous locations all through the rural area, providing an example of ancient living. 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Settlements\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\"},\"id\":3739,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\",\"name\":\"\\u039f\\u03b9\\u03ba\\u03b9\\u03c3\\u03bc\\u03bf\\u03af\",\"id\":\"10\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Kaminia\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Kaminia\\\" width=\\\"300\\\" height=\\\"193\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u0391\\u039c\\u0399\\u039d\\u0399\\u0391_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kaminia\\\/\\\">Kaminia<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kaminia\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>According to tradition, the settlement was founded on the Vroskopos coastline, where Byzantine cemeteries have been discovered. The existence of kilns, in which clay pots were made or metal was melted, gave the village its name. Excavations began in the 1920s and 1930s, revealing the prehistoric city of Poliochni. There are a number of noteworthy [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8633\",\"lng\":\"25.3198\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kaminia\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>According to tradition, the settlement was founded on the Vroskopos coastline, where Byzantine cemeteries have been discovered. The existence of kilns, in which clay pots were made or metal was melted, gave the village its name. Excavations began in the 1920s and 1930s, revealing the prehistoric city of Poliochni. There are a number of noteworthy [&hellip;]<\\\/p>\\n\",\"post_content\":\"According to tradition, the settlement was founded on the Vroskopos coastline, where Byzantine cemeteries have been discovered. The existence of kilns, in which clay pots were made or metal was melted, gave the village its name. Excavations began in the 1920s and 1930s, revealing the prehistoric city of Poliochni. There are a number of noteworthy attractions in the Kaminia area. The carved Pelasgian graves, the \\\"Column of the Furnaces,\\\" as well as the Holy Church of the Assumption completed in 1852, the Old Fountain with the built-in Turkish inscription, the Statue of the historian Argyrios Moshidis, and the cobbled plaza are all worth seeing.\\r\\n\\r\\nMany historic chapels may be found in Kaminia: Ag. Alexandros Sokastrou (1930), Ag. Alexandros Angona (1911), Ag. Alexandros Merpia (before 1900), Ag. Varvara (before 1917), Ag. Vlasis (before 1900), Ag. Giorgios Vroskopou, Ag. Giorgios Limaniou (1882), Ag. Giannis Mesarahis (1873), Ag. Giannis Kaminiotis (1881), Ag. Dimitrios (1884), Agios Nikolaos (1861), and Kato Panagia (1899).\\r\\n\\r\\nXespasmata, Molos, and Kokkinovrahos \\\/ Ag. Triada are some of the area's most stunning beaches.\",\"post_title\":\"Kaminia\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kaminia\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Kaminia\\\" width=\\\"300\\\" height=\\\"193\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u0391\\u039c\\u0399\\u039d\\u0399\\u0391_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"10\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.8633\",\"%_wpgmp_metabox_longitude%\":\"25.3198\",\"%wpcf-latitude%\":\"39.8633\",\"%wpcf-longtitude%\":\"25.3198\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses-1.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2921\",\"%_edit_lock%\":\"1661173293:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%ba%ce%b1%ce%bc%ce%af%ce%bd%ce%b9%ce%b1\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u0391\\u039c\\u0399\\u039d\\u0399\\u0391_001.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"23462\",\"%wpcf-code%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039a\\u0391\\u039c\\u0399\\u039d\\u0399\\u0391_001.jpg, \\u039a\\u0391\\u039c\\u0399\\u039d\\u0399\\u0391_001, \",\"%_et_pb_truncate_post%\":\"<p>According to tradition, the settlement was founded on the Vroskopos coastline, where Byzantine cemeteries have been discovered. The existence of kilns, in which clay pots were made or metal was melted, gave the village its name. Excavations began in the 1920s and 1930s, revealing the prehistoric city of Poliochni. There are a number of noteworthy attractions in the Kaminia area. The carved Pelasgian graves, the &#8220;Column of the Furnaces,&#8221; as well as the Holy Church of the Assumption completed in 1852, the Old Fountain with the built-in Turkish inscription, the Statue of the historian Argyrios Moshidis, and the cobbled plaza are all worth seeing.<\\\/p>\\n<p>Many historic chapels may be found in Kaminia: Ag. Alexandros Sokastrou (1930), Ag. Alexandros Angona (1911), Ag. Alexandros Merpia (before 1900), Ag. Varvara (before 1917), Ag. Vlasis (before 1900), Ag. Giorgios Vroskopou, Ag. Giorgios Limaniou (1882), Ag. Giannis Mesarahis (1873), Ag. Giannis Kaminiotis (1881), Ag. Dimitrios (1884), Agios Nikolaos (1861), and Kato Panagia (1899).<\\\/p>\\n<p>Xespasmata, Molos, and Kokkinovrahos \\\/ Ag. 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Settlements\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\"},\"id\":3746,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\",\"name\":\"\\u039f\\u03b9\\u03ba\\u03b9\\u03c3\\u03bc\\u03bf\\u03af\",\"id\":\"10\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Fisini\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Fisini\\\" width=\\\"300\\\" height=\\\"193\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a6\\u0399\\u03a3\\u0399\\u039d\\u0397_002-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/fisini\\\/\\\">Fisini<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/fisini\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The settlement is referred to as Vishin (in 1856), Fsin or Psin, and its residents as Sfnades in local dialect and community documentation from the 19th century. As a result, the feminine form of the name\\u00a0prevailed: Fisini, which was assigned to the word \\\"fyso\\\" (blow)\\u00a0via folk etymology, since \\\"f'sa, sfniz\\\": as the area is exposed [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8149\",\"lng\":\"25.3445\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/fisini\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The settlement is referred to as Vishin (in 1856), Fsin or Psin, and its residents as Sfnades in local dialect and community documentation from the 19th century. As a result, the feminine form of the name\\u00a0prevailed: Fisini, which was assigned to the word \\\"fyso\\\" (blow)\\u00a0via folk etymology, since \\\"f'sa, sfniz\\\": as the area is exposed [&hellip;]<\\\/p>\\n\",\"post_content\":\"The settlement is referred to as Vishin (in 1856), Fsin or Psin, and its residents as Sfnades in local dialect and community documentation from the 19th century. As a result, the feminine form of the name\\u00a0prevailed: Fisini, which was assigned to the word \\\"fyso\\\" (blow)\\u00a0via folk etymology, since \\\"f'sa, sfniz\\\": as the area is exposed to strong winds.\\r\\n\\r\\nAgios Alexandros was Lemnos' patron saint during the Byzantine era, and his relics were held on the island until 1308. His body, however, was taken and carried to Venice during a pirate attack. The veneration of Agios Alexandros as the patron saint of Lemnos has waned since then.\\r\\n\\r\\nSt. Sofia\\r\\n\\r\\nSince the establishment of municipalities and communities in 1918 (Government Decree 116 A),the St.Sofia has always been a part of the Fisini community. Composed of the villages of Skala, the neighbouring mediaeval castle, Skandali, and its residents that were known as Skaliotes.\\r\\n\\r\\nThere are ruins of mediaeval structures at two locations surrounding the settlement: Parthenomtos, west of the settlement, from which the residents fled and moved to\\u00a0Skandali, and Agiomarnos, east of the village, near the seaside,\\u00a0where ruins of residences as well as churches can be found.\\r\\n\\r\\nThe Paradisi hill (286 m.) that overlooks southeastern Lemnos is located on the outskirts of the settlement. On its slopes, fossilised tree trunks have been revealed, as well as meadows that are home to beehives, rabbits and pheasants. As a result, a major portion of it has been established as a hunting preserve.\",\"post_title\":\"Fisini\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/fisini\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Fisini\\\" width=\\\"300\\\" height=\\\"193\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a6\\u0399\\u03a3\\u0399\\u039d\\u0397_002-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"10\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.8149\",\"%_wpgmp_metabox_longitude%\":\"25.3445\",\"%wpcf-latitude%\":\"39.8149\",\"%wpcf-longtitude%\":\"25.3445\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses-1.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2894\",\"%_edit_lock%\":\"1661173558:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%86%ce%b9%cf%83%ce%af%ce%bd%ce%b7\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a6\\u0399\\u03a3\\u0399\\u039d\\u0397_001.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"23501, 23502\",\"%wpcf-code%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a6\\u0399\\u03a3\\u0399\\u039d\\u0397_002.jpg, \\u03a6\\u0399\\u03a3\\u0399\\u039d\\u0397_002, \",\"%_et_pb_truncate_post%\":\"<p>The settlement is referred to as Vishin (in 1856), Fsin or Psin, and its residents as Sfnades in local dialect and community documentation from the 19th century. As a result, the feminine form of the name\\u00a0prevailed: Fisini, which was assigned to the word &#8220;fyso&#8221; (blow)\\u00a0via folk etymology, since &#8220;f&#8217;sa, sfniz&#8221;: as the area is exposed to strong winds.<\\\/p>\\n<p>Agios Alexandros was Lemnos&#8217; patron saint during the Byzantine era, and his relics were held on the island until 1308. His body, however, was taken and carried to Venice during a pirate attack. The veneration of Agios Alexandros as the patron saint of Lemnos has waned since then.<\\\/p>\\n<p>St. Sofia<\\\/p>\\n<p>Since the establishment of municipalities and communities in 1918 (Government Decree 116 A),the St.Sofia has always been a part of the Fisini community. Composed of the villages of Skala, the neighbouring mediaeval castle, Skandali, and its residents that were known as Skaliotes.<\\\/p>\\n<p>There are ruins of mediaeval structures at two locations surrounding the settlement: Parthenomtos, west of the settlement, from which the residents fled and moved to\\u00a0Skandali, and Agiomarnos, east of the village, near the seaside,\\u00a0where ruins of residences as well as churches can be found.<\\\/p>\\n<p>The Paradisi hill (286 m.) that overlooks southeastern Lemnos is located on the outskirts of the settlement. On its slopes, fossilised tree trunks have been revealed, as well as meadows that are home to beehives, rabbits and pheasants. 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class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/skandali\\\/\\\">Skandali<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/skandali\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>In 1321, the town was first recognized as one of 25 patriarchal exarchates on the island of Lemnos. 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It is so effectively concealed that the visitor does not see it until reaching the top of the overlooking\\u00a0hill. Many people lived on the island's north shore, in Gomati, before migrating to Katalakkos\\u00a0for safety from piracy threats. The local church, Agios Modestos, was constructed by the residents in 1856 with\\u00a0their own money and effort. It features a basic gabled roof and colourful wood-carved shields that date from the early twentieth century. 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fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/sardes\\\/\\\">Sardes<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/sardes\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The community is named after the Byzantine settlement Ardia or Ardeia, which was located in the northern part of Lemnos. 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Settlements\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\"},\"id\":3751,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/houses_result-2-small.png\",\"name\":\"\\u039f\\u03b9\\u03ba\\u03b9\\u03c3\\u03bc\\u03bf\\u03af\",\"id\":\"10\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"The Medieval Castle of Myrina\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"The Medieval Castle of Myrina\\\" width=\\\"300\\\" height=\\\"136\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039c\\u0395\\u03a3\\u0391\\u0399\\u03a9\\u039d\\u0399\\u039a\\u039f-\\u039a\\u0391\\u03a3\\u03a4\\u03a1\\u039f-\\u039c\\u03a5\\u03a1\\u0399\\u039d\\u0391\\u03a3_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-medieval-castle-of-myrina\\\/\\\">The Medieval Castle of Myrina<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-medieval-castle-of-myrina\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The medieval castle of Myrina is built on the steep and rocky peninsula of the town of Myrina. This structure is one of the largest forts in the Aegean region, as its positioning allows the control of the two bays of Myrina. There was an old citadel with cyclopean walls on the site of the [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8776\",\"lng\":\"25.0552\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-medieval-castle-of-myrina\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The medieval castle of Myrina is built on the steep and rocky peninsula of the town of Myrina. This structure is one of the largest forts in the Aegean region, as its positioning allows the control of the two bays of Myrina. There was an old citadel with cyclopean walls on the site of the [&hellip;]<\\\/p>\\n\",\"post_content\":\"The medieval castle of Myrina is built on the steep and rocky peninsula of the town of Myrina. This structure is one of the largest forts in the Aegean region, as its positioning allows the control of the two bays of Myrina.\\r\\n\\r\\nThere was an old citadel with cyclopean walls on the site of the castle, dating back to the 13<sup>th<\\\/sup> century BC. The Pelasgians captured Lemnos in the 8<sup>th<\\\/sup> century BC, strengthening the castle's fortifications (sources mention the Pelasgian citadel in Myrina).\\r\\n\\r\\nThe castle was constructed in the early 12<sup>th<\\\/sup> century AD (Byzantine period) with material from the old citadel, and its defenses were reinforced in 1185 by Emperor Andronikos I Komnenos.\\r\\n\\r\\nIt was fortified in 1207 by the Venetian Philokalos Navigagiozo, Grand Duke of Lemnos (in which form we see it today). Turks resided within the castle during the Turkish occupation. During the Russian fleet's siege of Myrina in 1770, the castle walls were damaged.\\r\\n\\r\\nCovering an area of 144 acres, the castle has a triple wall with 14 towers and two gates, the main gate facing eastwards, and the smaller one facing westwards. The higher wall to the east and south has numerous towers, while the lower northern and western walls have fewer towers.\\r\\n\\r\\nThe remnants of a fortified building with multiple rooms may be seen at the highest point of the hill. Finally, a Turkish mosque, an underground vaulted chamber, and water\\u00a0cisterns can also be found within the castle.\",\"post_title\":\"The Medieval Castle of Myrina\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-medieval-castle-of-myrina\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"The Medieval Castle of Myrina\\\" width=\\\"300\\\" height=\\\"136\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039c\\u0395\\u03a3\\u0391\\u0399\\u03a9\\u039d\\u0399\\u039a\\u039f-\\u039a\\u0391\\u03a3\\u03a4\\u03a1\\u039f-\\u039c\\u03a5\\u03a1\\u0399\\u039d\\u0391\\u03a3_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"7\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.8776\",\"%_wpgmp_metabox_longitude%\":\"25.0552\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2848\",\"%_edit_lock%\":\"1657792289:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%bc%ce%b5%cf%83%ce%b1%ce%b9%cf%89%ce%bd%ce%b9%ce%ba%cf%8c-%ce%ba%ce%ac%cf%83%cf%84%cf%81%ce%bf-%ce%bc%cf%8d%cf%81%ce%b9%ce%bd%ce%b1%cf%82-%ce%bd-%ce%bb%ce%ae%ce%bc%ce%bd%ce%bf%cf%85\",\"%wpcf-latitude%\":\"\",\"%wpcf-longtitude%\":\"\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039c\\u0395\\u03a3\\u0391\\u0399\\u03a9\\u039d\\u0399\\u039a\\u039f-\\u039a\\u0391\\u03a3\\u03a4\\u03a1\\u039f-\\u039c\\u03a5\\u03a1\\u0399\\u039d\\u0391\\u03a3_001.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"21320, 21321, 21322, 21323, 21324\",\"%wpcf-code%\":\"\",\"%wpcf-mapicon%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u039c\\u0395\\u03a3\\u0391\\u0399\\u03a9\\u039d\\u0399\\u039a\\u039f-\\u039a\\u0391\\u03a3\\u03a4\\u03a1\\u039f-\\u039c\\u03a5\\u03a1\\u0399\\u039d\\u0391\\u03a3_005.jpg, \\u039c\\u0395\\u03a3\\u0391\\u0399\\u03a9\\u039d\\u0399\\u039a\\u039f \\u039a\\u0391\\u03a3\\u03a4\\u03a1\\u039f \\u039c\\u03a5\\u03a1\\u0399\\u039d\\u0391\\u03a3_005, \",\"%_et_pb_truncate_post%\":\"<p>The medieval castle of Myrina is built on the steep and rocky peninsula of the town of Myrina. This structure is one of the largest forts in the Aegean region, as its positioning allows the control of the two bays of Myrina.<\\\/p>\\n<p>There was an old citadel with cyclopean walls on the site of the castle, dating back to the 13th century BC. The Pelasgians captured Lemnos in the 8th century BC, strengthening the castle&#8217;s fortifications (sources mention the Pelasgian citadel in Myrina).<\\\/p>\\n<p>The castle was constructed in the early 12th century AD (Byzantine period) with material from the old citadel, and its defenses were reinforced in 1185 by Emperor Andronikos I Komnenos.<\\\/p>\\n<p>It was fortified in 1207 by the Venetian Philokalos Navigagiozo, Grand Duke of Lemnos (in which form we see it today). Turks resided within the castle during the Turkish occupation. During the Russian fleet&#8217;s siege of Myrina in 1770, the castle walls were damaged.<\\\/p>\\n<p>Covering an area of 144 acres, the castle has a triple wall with 14 towers and two gates, the main gate facing eastwards, and the smaller one facing westwards. The higher wall to the east and south has numerous towers, while the lower northern and western walls have fewer towers.<\\\/p>\\n<p>The remnants of a fortified building with multiple rooms may be seen at the highest point of the hill. 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The city-state was the center of the ancient Greek religion, as the city was named after its protector the god Hephaestus. Coins discovered at the site, one of which depicts a burning [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9645\",\"lng\":\"25.3181\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/hephaistia\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>One of ancient Lemnos' two city-states, Hephaistia\\u2019s prosperity lasted from the 7th to the 1st century BC according to excavations and historical records. The city-state was the center of the ancient Greek religion, as the city was named after its protector the god Hephaestus. Coins discovered at the site, one of which depicts a burning [&hellip;]<\\\/p>\\n\",\"post_content\":\"One of ancient Lemnos' two city-states, Hephaistia\\u2019s prosperity lasted from the 7<sup>th<\\\/sup> to the 1<sup>st<\\\/sup> century BC according to excavations and historical records. The city-state was the center of the ancient Greek religion, as the city was named after its protector the god Hephaestus. Coins discovered at the site, one of which depicts a burning torch on one side, suggest that \\\"Hephaistia\\\" festivals were performed in honor of Hephaestus.\\r\\n\\r\\nEstablished by the Pelasgians on a peninsula that allowed them easy control over the two naturally created harbours, Hephaistia was a major port.\\r\\n\\r\\nNumerous tombs with pottery have been discovered, the oldest of which dates to\\u00a0the first part of the 5<sup>th<\\\/sup> century, with additional tombs dating back to Roman times. Among the Greek structures is the theater constructed during the Hellenistic era using Roman materials. The temples and houses, among other structures excavated, attest to the prominence of this city throughout the Byzantine period.\\r\\n\\r\\nTwo factors contributed to the downfall and eventual abandonment of Hephaistia: first, the loss of the port as a result of alluvial deposits following the frequent intense rainfall, and second, the prevalence of Christianity in the 2<sup>nd<\\\/sup> to 3<sup>rd<\\\/sup> century. Unable to practice their religion freely, the Christians sought a new base in Kotsino, the success of which accelerated Hephaistias' demise.\",\"post_title\":\"Hephaistia\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/hephaistia\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Hephaistia\\\" width=\\\"300\\\" height=\\\"151\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0397\\u03a6\\u0391\\u0399\\u03a3\\u03a4\\u0399\\u0391_002-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"7\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.9645\",\"%_wpgmp_metabox_longitude%\":\"25.3181\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2853\",\"%_edit_lock%\":\"1657801903:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%b7-%ce%b7%cf%86%ce%b1%ce%b9%cf%83%cf%84%ce%af%ce%b1\",\"%wpcf-latitude%\":\"\",\"%wpcf-longtitude%\":\"\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0397\\u03a6\\u0391\\u0399\\u03a3\\u03a4\\u0399\\u0391_002.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"21360\",\"%wpcf-code%\":\"\",\"%wpcf-mapicon%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0397\\u03a6\\u0391\\u0399\\u03a3\\u03a4\\u0399\\u0391_002.jpg, \\u0397\\u03a6\\u0391\\u0399\\u03a3\\u03a4\\u0399\\u0391_002, \",\"%_et_pb_truncate_post%\":\"<p>One of ancient Lemnos&#8217; two city-states, Hephaistia\\u2019s prosperity lasted from the 7th to the 1st century BC according to excavations and historical records. The city-state was the center of the ancient Greek religion, as the city was named after its protector the god Hephaestus. Coins discovered at the site, one of which depicts a burning torch on one side, suggest that &#8220;Hephaistia&#8221; festivals were performed in honor of Hephaestus.<\\\/p>\\n<p>Established by the Pelasgians on a peninsula that allowed them easy control over the two naturally created harbours, Hephaistia was a major port.<\\\/p>\\n<p>Numerous tombs with pottery have been discovered, the oldest of which dates to\\u00a0the first part of the 5th century, with additional tombs dating back to Roman times. Among the Greek structures is the theater constructed during the Hellenistic era using Roman materials. 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Poliochni was a settlement built between two streams, Psathia to the north and Avlaki to the south, upon a hill on a small peninsula stretching into the sea. Due to exposure to sea erosion, a large portion of the settlement has [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8535\",\"lng\":\"25.3426\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/poliochni-of-lemnos\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Poliochni is found on the east coast of Lemnos, in the bay of Vroskopos. Poliochni was a settlement built between two streams, Psathia to the north and Avlaki to the south, upon a hill on a small peninsula stretching into the sea. Due to exposure to sea erosion, a large portion of the settlement has [&hellip;]<\\\/p>\\n\",\"post_content\":\"Poliochni is found on the east coast of Lemnos, in the bay of Vroskopos. 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src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u03a1\\u03a7\\u0391\\u0399\\u039f\\u039b\\u039f\\u0393\\u0399\\u039a\\u039f\\u03a3-\\u03a7\\u03a9\\u03a1\\u039f\\u03a3-\\u03a0\\u03a1\\u039f\\u0399\\u03a3\\u03a4\\u039f\\u03a1\\u0399\\u039a\\u039f\\u03a5-\\u039f\\u0399\\u039a\\u0399\\u03a3\\u039c\\u039f\\u03a5-\\u039c\\u03a5\\u03a1\\u0399\\u039d\\u0391\\u03a3_003-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/archaeological-site-of-the-prehistoric-settlement-of-myrina-lemnos\\\/\\\">Archaeological Site of the Prehistoric Settlement of Myrina, Lemnos<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/archaeological-site-of-the-prehistoric-settlement-of-myrina-lemnos\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The archaeological site of the prehistoric settlement of Myrina is located on the wide 80.000 m2 coastal region, west of Myrina. The settlement was revealed in 1986 by an excavation carried out by the Ephorate of Prehistoric and Classical Antiquities. This prehistoric settlement existed simultaneously with the settlement of Poliochni, but according to the excavation [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8829\",\"lng\":\"25.0641\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/archaeological-site-of-the-prehistoric-settlement-of-myrina-lemnos\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The archaeological site of the prehistoric settlement of Myrina is located on the wide 80.000 m2 coastal region, west of Myrina. The settlement was revealed in 1986 by an excavation carried out by the Ephorate of Prehistoric and Classical Antiquities. 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sites\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/monuments_result-small.png\"},\"id\":3659,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/monuments_result-small.png\",\"name\":\"\\u0391\\u03c1\\u03c7\\u03b1\\u03b9\\u03bf\\u03bb\\u03bf\\u03b3\\u03b9\\u03ba\\u03bf\\u03af \\u03c7\\u03ce\\u03c1\\u03bf\\u03b9\",\"id\":\"7\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Temple of Kabeiri, Lemnos\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Temple of Kabeiri, Lemnos\\\" width=\\\"300\\\" height=\\\"136\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0399\\u0395\\u03a1\\u039f-\\u03a4\\u03a9\\u039d-\\u039a\\u0391\\u0392\\u0395\\u0399\\u03a1\\u03a9\\u039d_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding 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The temple went through three construction phases: the Archaic, the Hellenistic, and the late Roman. \\u00a0The temple\\u2019s buildings are found on two small terraces. Administratively part of Hephaistia, the Temple of Kabeiri was the center of the [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9792\",\"lng\":\"25.3416\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/temple-of-kabeiri-lemnos\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The Temple o Kabeiri was brought to light by the Italian Archeological School in the period of 1937-1991. The temple went through three construction phases: the Archaic, the Hellenistic, and the late Roman. \\u00a0The temple\\u2019s buildings are found on two small terraces. Administratively part of Hephaistia, the Temple of Kabeiri was the center of the [&hellip;]<\\\/p>\\n\",\"post_content\":\"The Temple o Kabeiri was brought to light by the Italian Archeological School in the period of 1937-1991. The temple went through three construction phases: the Archaic, the Hellenistic, and the late Roman. \\u00a0The temple\\u2019s buildings are found on two small terraces. Administratively part of Hephaistia, the Temple of Kabeiri was the center of the island as well as the center of worship.\\r\\n\\r\\nOn the southern plateau, an archaic telesterion was found under the late-Roman telesterion. It is a irregular rectangular building with counters upon which rituals were carried out, and it dates back to the beginning of the 7<sup>th<\\\/sup> century BC.\\r\\n\\r\\nThe northern plateau is occupied by the Hellenistic telesterion. It is a building with twelve Doric columns dating back the 2<sup>nd<\\\/sup> century BC. It was looted and burned during the Roman imperial period, between the 2<sup>nd<\\\/sup> and 3<sup>rd<\\\/sup> century AD.\\r\\n\\r\\nThe late-Roman telesterion is located on the southern plateau, and is built on the archaic building of the older archaic telesterion. The entrance to this telesterion was on the southern side and had a pronaos with 7 columns. The central hall was 17 m long and was separated into three sections. The ruins of this building represent the final phase of existence of the temple, and thus testify to the long survival of the Kabeiri worship. The destruction of the building and the termination of the temple were most likely caused by the destructive frenzy of the early Christians at the end of the 3<sup>rd<\\\/sup> or beginning of the 4<sup>th<\\\/sup> century AD.\",\"post_title\":\"Temple of Kabeiri, Lemnos\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/temple-of-kabeiri-lemnos\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Temple of Kabeiri, Lemnos\\\" width=\\\"300\\\" height=\\\"136\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0399\\u0395\\u03a1\\u039f-\\u03a4\\u03a9\\u039d-\\u039a\\u0391\\u0392\\u0395\\u0399\\u03a1\\u03a9\\u039d_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"7\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.9792\",\"%_wpgmp_metabox_longitude%\":\"25.3416\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2859\",\"%_edit_lock%\":\"1657802959:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%b9%ce%b5%cf%81%cf%8c-%cf%84%cf%89%ce%bd-%ce%ba%ce%b1%ce%b2%ce%b5%ce%af%cf%81%cf%89%ce%bd-%ce%bb%ce%ae%ce%bc%ce%bd%ce%bf%cf%85\",\"%wpcf-latitude%\":\"\",\"%wpcf-longtitude%\":\"\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0399\\u0395\\u03a1\\u039f-\\u03a4\\u03a9\\u039d-\\u039a\\u0391\\u0392\\u0395\\u0399\\u03a1\\u03a9\\u039d_001.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"21476\",\"%wpcf-code%\":\"\",\"%wpcf-mapicon%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0399\\u0395\\u03a1\\u039f-\\u03a4\\u03a9\\u039d-\\u039a\\u0391\\u0392\\u0395\\u0399\\u03a1\\u03a9\\u039d_001.jpg, \\u0399\\u0395\\u03a1\\u039f \\u03a4\\u03a9\\u039d \\u039a\\u0391\\u0392\\u0395\\u0399\\u03a1\\u03a9\\u039d_001, \",\"%_et_pb_truncate_post%\":\"<p>The Temple o Kabeiri was brought to light by the Italian Archeological School in the period of 1937-1991. The temple went through three construction phases: the Archaic, the Hellenistic, and the late Roman. \\u00a0The temple\\u2019s buildings are found on two small terraces. Administratively part of Hephaistia, the Temple of Kabeiri was the center of the island as well as the center of worship.<\\\/p>\\n<p>On the southern plateau, an archaic telesterion was found under the late-Roman telesterion. It is a irregular rectangular building with counters upon which rituals were carried out, and it dates back to the beginning of the 7th century BC.<\\\/p>\\n<p>The northern plateau is occupied by the Hellenistic telesterion. It is a building with twelve Doric columns dating back the 2nd century BC. It was looted and burned during the Roman imperial period, between the 2nd and 3rd century AD.<\\\/p>\\n<p>The late-Roman telesterion is located on the southern plateau, and is built on the archaic building of the older archaic telesterion. The entrance to this telesterion was on the southern side and had a pronaos with 7 columns. The central hall was 17 m long and was separated into three sections. The ruins of this building represent the final phase of existence of the temple, and thus testify to the long survival of the Kabeiri worship. 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sites\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/monuments_result-small.png\"},\"id\":3661,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/monuments_result-small.png\",\"name\":\"\\u0391\\u03c1\\u03c7\\u03b1\\u03b9\\u03bf\\u03bb\\u03bf\\u03b3\\u03b9\\u03ba\\u03bf\\u03af \\u03c7\\u03ce\\u03c1\\u03bf\\u03b9\",\"id\":\"7\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"The Philoctetes Cave\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"The Philoctetes Cave\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a3\\u03a0\\u0397\\u039b\\u0399\\u0391-\\u03a4\\u039f\\u03a5-\\u03a6\\u0399\\u039b\\u039f\\u039a\\u03a4\\u0397\\u03a4\\u0397_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-philoctetes-cave\\\/\\\">The Philoctetes Cave<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-philoctetes-cave\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Located in the NE region of the island, the Philoctetes Cave is found under one of the most important archaeological sites of Lemnos, the Kaveira site. By following a small, narrow path down to the shore, the visitor will be greeted by a big cavern with a big overhead opening that extends into the sea. [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9795\",\"lng\":\"25.3409\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-philoctetes-cave\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Located in the NE region of the island, the Philoctetes Cave is found under one of the most important archaeological sites of Lemnos, the Kaveira site. By following a small, narrow path down to the shore, the visitor will be greeted by a big cavern with a big overhead opening that extends into the sea. [&hellip;]<\\\/p>\\n\",\"post_content\":\"Located in the NE region of the island, the Philoctetes Cave is found under one of the most important archaeological sites of Lemnos, the Kaveira site. By following a small, narrow path down to the shore, the visitor will be greeted by a big cavern with a big overhead opening that extends into the sea. This path is not the only entrance into the cave.\\r\\n\\r\\nIn Greek mythology, Philoctetes was the hero to whom Hercules gave his bow and arrows. According to legend, Philoctetes was healed from a snake bite by staying in the cave for ten years and by the healing powers of Lemnian Earth. And finally, when the Achaeans required Philoctetes' assistance to conquer Troy and bring the lengthy war to an end, they returned to Lemnos and begged Philoctetes for forgiveness.\",\"post_title\":\"The Philoctetes Cave\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-philoctetes-cave\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"The Philoctetes Cave\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a3\\u03a0\\u0397\\u039b\\u0399\\u0391-\\u03a4\\u039f\\u03a5-\\u03a6\\u0399\\u039b\\u039f\\u039a\\u03a4\\u0397\\u03a4\\u0397_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"7\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.9795\",\"%_wpgmp_metabox_longitude%\":\"25.3409\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2856\",\"%_edit_lock%\":\"1657802954:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%b7-%cf%83%cf%80%ce%b7%ce%bb%ce%b9%ce%ac-%cf%84%ce%bf%cf%85-%cf%86%ce%b9%ce%bb%ce%bf%ce%ba%cf%84%ce%ae%cf%84%ce%b7\",\"%wpcf-latitude%\":\"\",\"%wpcf-longtitude%\":\"\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a3\\u03a0\\u0397\\u039b\\u0399\\u0391-\\u03a4\\u039f\\u03a5-\\u03a6\\u0399\\u039b\\u039f\\u039a\\u03a4\\u0397\\u03a4\\u0397_001.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"21513, 21514\",\"%wpcf-code%\":\"\",\"%wpcf-mapicon%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a3\\u03a0\\u0397\\u039b\\u0399\\u0391-\\u03a4\\u039f\\u03a5-\\u03a6\\u0399\\u039b\\u039f\\u039a\\u03a4\\u0397\\u03a4\\u0397_002.jpg, \\u03a3\\u03a0\\u0397\\u039b\\u0399\\u0391 \\u03a4\\u039f\\u03a5 \\u03a6\\u0399\\u039b\\u039f\\u039a\\u03a4\\u0397\\u03a4\\u0397_002, \",\"%_et_pb_truncate_post%\":\"<p>Located in the NE region of the island, the Philoctetes Cave is found under one of the most important archaeological sites of Lemnos, the Kaveira site. By following a small, narrow path down to the shore, the visitor will be greeted by a big cavern with a big overhead opening that extends into the sea. This path is not the only entrance into the cave.<\\\/p>\\n<p>In Greek mythology, Philoctetes was the hero to whom Hercules gave his bow and arrows. According to legend, Philoctetes was healed from a snake bite by staying in the cave for ten years and by the healing powers of Lemnian Earth. 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Archaeological and epigraphic evidence backs up the identification of a large Artemis temple which was found on the site of the Porto Myrina Hotel and is now preserved inside the hotel complex. The site was excavated between 1991-1993 at the expense of the [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8935\",\"lng\":\"25.0624\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/temple-of-artemis-in-avlona-myrina\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>In ancient times, Artemis was the protector of the city of Myrina. Archaeological and epigraphic evidence backs up the identification of a large Artemis temple which was found on the site of the Porto Myrina Hotel and is now preserved inside the hotel complex. The site was excavated between 1991-1993 at the expense of the [&hellip;]<\\\/p>\\n\",\"post_content\":\"In ancient times, Artemis was the protector of the city of Myrina. Archaeological and epigraphic evidence backs up the identification of a large Artemis temple which was found on the site of the Porto Myrina Hotel and is now preserved inside the hotel complex.\\r\\n\\r\\nThe site was excavated between 1991-1993 at the expense of the owner N. Tratarou. A large, central outdoor cobblestoned courtyard is included in the property. There were secondary chambers around the courtyard that were once utilized by the priests\\u00a0for storage supplies and the basic day-to-day operations of the temple. The sanctuary was enclosed by a double \\\"wall,\\\" and had two entrances, one viewing the city and the other the sea, which can indicate the existence of a small port in the bay. There were also three wells, as worship water was required for the rites. 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Archaeological and epigraphic evidence backs up the identification of a large Artemis temple which was found on the site of the Porto Myrina Hotel and is now preserved inside the hotel complex.<\\\/p>\\n<p>The site was excavated between 1991-1993 at the expense of the owner N. Tratarou. A large, central outdoor cobblestoned courtyard is included in the property. There were secondary chambers around the courtyard that were once utilized by the priests\\u00a0for storage supplies and the basic day-to-day operations of the temple. The sanctuary was enclosed by a double &#8220;wall,&#8221; and had two entrances, one viewing the city and the other the sea, which can indicate the existence of a small port in the bay. There were also three wells, as worship water was required for the rites. 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It is located in the city center and is regarded as the city's second most important church after the Evangelistria. It was constructed in 1835 and is three-aisled with an exonarthex, built later, while previous stages of the church date back to [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8746\",\"lng\":\"25.2675\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/taxiarchis-moudrou\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The Taxiarchis Moudrou Church is also known as the Temple of the Archangels. It is located in the city center and is regarded as the city's second most important church after the Evangelistria. It was constructed in 1835 and is three-aisled with an exonarthex, built later, while previous stages of the church date back to [&hellip;]<\\\/p>\\n\",\"post_content\":\"The Taxiarchis Moudrou Church is also known as the Temple of the Archangels. 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monuments\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/church_result-small.png\"},\"id\":3671,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/church_result-small.png\",\"name\":\"\\u0398\\u03c1\\u03b7\\u03c3\\u03ba\\u03b5\\u03c5\\u03c4\\u03b9\\u03ba\\u03ac \\u03bc\\u03bd\\u03b7\\u03bc\\u03b5\\u03af\\u03b1\",\"id\":\"8\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Virgin Mary of Trigi\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Virgin Mary of Trigi\\\" width=\\\"300\\\" height=\\\"199\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u0391\\u039d\\u0391\\u0393\\u0399\\u0391-\\u03a3\\u03a4\\u0397\\u039d-\\u03a4\\u03a1\\u03a5\\u0393\\u0397_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/virgin-mary-of-trigi\\\/\\\">Virgin Mary of Trigi<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/virgin-mary-of-trigi\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The Church of the Virgin Mary in Trigi is one of the most important chapels of Lemnos as it dates to the 14th century. References to the chapel, which then was a monastery, date back to 1364 as it is referred to as a part of Simon Petra of Mount Athos. According to different reports, [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9778\",\"lng\":\"25.2540\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/virgin-mary-of-trigi\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The Church of the Virgin Mary in Trigi is one of the most important chapels of Lemnos as it dates to the 14th century. References to the chapel, which then was a monastery, date back to 1364 as it is referred to as a part of Simon Petra of Mount Athos. According to different reports, [&hellip;]<\\\/p>\\n\",\"post_content\":\"The Church of the Virgin Mary in Trigi is one of the most important chapels of Lemnos as it dates to the 14<sup>th<\\\/sup> century. References to the chapel, which then was a monastery, date back to 1364 as it is referred to as a part of Simon Petra of Mount Athos. According to different reports, it was confirmed in 1798 by a patriarchal seal.\\r\\n\\r\\nOnly the eastern side of the original stonework of the Virgin Mary at Trygi is preserved, along with the three-sided altar and the inscription: \\\" CONSTRUCTED\\u2026 LOVED MONK OF AXIOTI\\u2026 IN THE YEAR 1706\\\" which suggests some sort of a renovation took place.\\r\\n\\r\\nOn the 15th of August, the Virgin Mary of Trigi is celebrated, and people from all over Lemnos gather to the scenic church. The images of the Virgin Mary are regarded as works of great art, while the icon of the Virgin Hodegetria, which has been housed there since 1700, is considered to cause miracles. The Virgin Mary is represented with a white garment, the color associated with purity, and how she reveals herself to the faithful.\",\"post_title\":\"Virgin Mary of Trigi\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/virgin-mary-of-trigi\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Virgin Mary of Trigi\\\" width=\\\"300\\\" height=\\\"199\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u0391\\u039d\\u0391\\u0393\\u0399\\u0391-\\u03a3\\u03a4\\u0397\\u039d-\\u03a4\\u03a1\\u03a5\\u0393\\u0397_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"8\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.9778\",\"%_wpgmp_metabox_longitude%\":\"25.2540\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2885\",\"%_edit_lock%\":\"1657872560:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%80%ce%b1%ce%bd%ce%b1%ce%b3%ce%af%ce%b1-%cf%83%cf%84%ce%b7%ce%bd-%cf%84%cf%81%cf%85%ce%b3%ce%ae\",\"%wpcf-latitude%\":\"\",\"%wpcf-longtitude%\":\"\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u0391\\u039d\\u0391\\u0393\\u0399\\u0391-\\u03a3\\u03a4\\u0397\\u039d-\\u03a4\\u03a1\\u03a5\\u0393\\u0397_001.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"21760, 21761, 21762\",\"%wpcf-code%\":\"\",\"%wpcf-mapicon%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u0391\\u039d\\u0391\\u0393\\u0399\\u0391-\\u03a3\\u03a4\\u0397\\u039d-\\u03a4\\u03a1\\u03a5\\u0393\\u0397_003.jpg, \\u03a0\\u0391\\u039d\\u0391\\u0393\\u0399\\u0391 \\u03a3\\u03a4\\u0397\\u039d \\u03a4\\u03a1\\u03a5\\u0393\\u0397_003, \",\"%_et_pb_truncate_post%\":\"<p>The Church of the Virgin Mary in Trigi is one of the most important chapels of Lemnos as it dates to the 14th century. 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monuments\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/church_result-small.png\"},\"id\":3673,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/church_result-small.png\",\"name\":\"\\u0398\\u03c1\\u03b7\\u03c3\\u03ba\\u03b5\\u03c5\\u03c4\\u03b9\\u03ba\\u03ac \\u03bc\\u03bd\\u03b7\\u03bc\\u03b5\\u03af\\u03b1\",\"id\":\"8\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Panagia Kakkaviotissa\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Panagia Kakkaviotissa\\\" width=\\\"300\\\" height=\\\"205\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u0391\\u039d\\u0391\\u0393\\u0399\\u0391-\\u039a\\u0391\\u039a\\u039a\\u0391\\u0392\\u0399\\u03a9\\u03a4\\u0399\\u03a3\\u03a3\\u0391_003-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/panagia-kakkaviotissa\\\/\\\">Panagia Kakkaviotissa<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/panagia-kakkaviotissa\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Panagia Kakkaviotissa is an impressive church located on the hill Kakkavos, about four kilometers from Myrina and the nearby Thanos village. Panagia Kakkaviotissa is built within the hollow of a\\u00a0rock, which \\\"serves\\\" as a roof for the little chapel because it lacks one. It originates from the early 14th century, when monks from Agios Efstratios [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8651\",\"lng\":\"25.1070\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/panagia-kakkaviotissa\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Panagia Kakkaviotissa is an impressive church located on the hill Kakkavos, about four kilometers from Myrina and the nearby Thanos village. Panagia Kakkaviotissa is built within the hollow of a\\u00a0rock, which \\\"serves\\\" as a roof for the little chapel because it lacks one. It originates from the early 14th century, when monks from Agios Efstratios [&hellip;]<\\\/p>\\n\",\"post_content\":\"Panagia Kakkaviotissa is an impressive church located on the hill Kakkavos, about four kilometers from Myrina and the nearby Thanos village.\\r\\n\\r\\nPanagia Kakkaviotissa is built within the hollow of a\\u00a0rock, which \\\"serves\\\" as a roof for the little chapel because it lacks one. It originates from the early 14th century, when monks from Agios Efstratios arrived and built it as part of the Monastery of the Great Lavra of Mount Athos.\\r\\n\\r\\nAccording to religious tradition and legend surrounding Panagia Kakkaviotissa, the last monk who left the chapel entrusted the picture of the Panagia to the Moumtzis family of Kontias, who still have it today. It is even reported that the monk then built a boat and set sail towards Mount Athos...\\r\\n\\r\\nEvery year on Easter Tuesday (Lambrotritis), the icon returns to Panagia Kakkaviotissa accompanied by a large number of believers and is solemnly honored.\",\"post_title\":\"Panagia Kakkaviotissa\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/panagia-kakkaviotissa\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Panagia Kakkaviotissa\\\" width=\\\"300\\\" height=\\\"205\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u0391\\u039d\\u0391\\u0393\\u0399\\u0391-\\u039a\\u0391\\u039a\\u039a\\u0391\\u0392\\u0399\\u03a9\\u03a4\\u0399\\u03a3\\u03a3\\u0391_003-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"8\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.8651\",\"%_wpgmp_metabox_longitude%\":\"25.1070\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2882\",\"%_edit_lock%\":\"1657873507:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%80%ce%b1%ce%bd%ce%b1%ce%b3%ce%af%ce%b1-%ce%ba%ce%b1%ce%ba%ce%ba%ce%b1%ce%b2%ce%b9%cf%8e%cf%84%ce%b9%cf%83%cf%83%ce%b1\",\"%wpcf-latitude%\":\"\",\"%wpcf-longtitude%\":\"\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u0391\\u039d\\u0391\\u0393\\u0399\\u0391-\\u039a\\u0391\\u039a\\u039a\\u0391\\u0392\\u0399\\u03a9\\u03a4\\u0399\\u03a3\\u03a3\\u0391_001.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"21802, 21803, 21804, 21805, 21806\",\"%wpcf-code%\":\"\",\"%wpcf-mapicon%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u03a0\\u0391\\u039d\\u0391\\u0393\\u0399\\u0391-\\u039a\\u0391\\u039a\\u039a\\u0391\\u0392\\u0399\\u03a9\\u03a4\\u0399\\u03a3\\u03a3\\u0391_005.jpg, \\u03a0\\u0391\\u039d\\u0391\\u0393\\u0399\\u0391 \\u039a\\u0391\\u039a\\u039a\\u0391\\u0392\\u0399\\u03a9\\u03a4\\u0399\\u03a3\\u03a3\\u0391_005, \",\"%_et_pb_truncate_post%\":\"<p>Panagia Kakkaviotissa is an impressive church located on the hill Kakkavos, about four kilometers from Myrina and the nearby Thanos village.<\\\/p>\\n<p>Panagia Kakkaviotissa is built within the hollow of a\\u00a0rock, which &#8220;serves&#8221; as a roof for the little chapel because it lacks one. 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It was built in 1830 and serves as the town cemetery church. The Church of the Nativity of Christ is a three-aisled basilica built in the local architectural style. The exonarthex's [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9052\",\"lng\":\"25.2893\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/church-of-the-nativity-of-christ\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The Church of the Nativity of Christ in the town of Romanou on Lemnos is one of the most remarkable structures in the area. It was built in 1830 and serves as the town cemetery church. The Church of the Nativity of Christ is a three-aisled basilica built in the local architectural style. The exonarthex's [&hellip;]<\\\/p>\\n\",\"post_content\":\"The Church of the Nativity of Christ in the town of Romanou on Lemnos is one of the most remarkable structures in the area. It was built in 1830 and serves as the town cemetery church. The Church of the Nativity of Christ is a three-aisled basilica built in the local architectural style. 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           <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/metropolis-of-lemnos\\\/\\\">Metropolis of Lemnos<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/metropolis-of-lemnos\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Built in 1864 in Myrina close to the rock bridge of the Trifoto area, the Metropolis of Lemnos is the church of the Holy Trinity. The project was carried out by the famous temple builder Zacharias Filippotis of Tinos and was funded by expatriates of Lemnos. The church itself was a three-aisled basilica with a [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8807\",\"lng\":\"25.0631\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/metropolis-of-lemnos\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Built in 1864 in Myrina close to the rock bridge of the Trifoto area, the Metropolis of Lemnos is the church of the Holy Trinity. The project was carried out by the famous temple builder Zacharias Filippotis of Tinos and was funded by expatriates of Lemnos. 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hill. References to the Zoodochos Pigi church can be traced back to the late Byzantine period when the island was under Venetian rule. [&hellip;]<\\\/p>\\n\",\"address\":\"Unnamed Road, Limnos 814 01, Greece\",\"location\":{\"lat\":\"39.9414\",\"city\":\"Limnos\",\"country\":\"Greece\",\"lng\":\"25.2853\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-zoodochos-pigi-kotsina\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The church of Zoodochos Pigi in Kotsina is one of the most interesting churches in Lemnos due to the underground tunnel that leads to the holy water in the heart of the hill. References to the Zoodochos Pigi church can be traced back to the late Byzantine period when the island was under Venetian rule. [&hellip;]<\\\/p>\\n\",\"post_content\":\"The church of Zoodochos Pigi in Kotsina is one of the most interesting churches in Lemnos due to the underground tunnel that leads to the holy water in the heart of the hill. References to the Zoodochos Pigi church can be traced back to the late Byzantine period when the island was under Venetian rule. Then, the church was located within the walls of the Castle of Kotsina, which was an important port on Lemnos at the time. It was initially dedicated to the Virgin Mary, but it is unknown how it eventually came to be dedicated to Zoodochos Pigi (\\u201cLife-giving well\\u201d). The current building of the church was constructed in the 1950s. To access the holy water of the church, visitors must descend approximately 60 steps down a domed tunnel to the center of the hill where there is a room that is below sea level. The Venetian builders of the Castle understood the value of the underground well, and they preserved it, making it accessible even today. Zoodochos Pigi Kotsina celebrates Easter Friday with a large festival in the church courtyard. A female statue may be seen in the courtyard of Zoodochos Pigi Kotsina.\\r\\n\\r\\nAccording to history, this is Maroula, the local hero who led her fellow villagers to drive out\\u00a0the Turks who had\\u00a0besieged the Castle in 1478.\",\"post_title\":\"The Church of Zoodochos Pigi Kotsina\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-zoodochos-pigi-kotsina\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"The Church of Zoodochos Pigi Kotsina\\\" width=\\\"300\\\" height=\\\"204\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0396\\u03a9\\u039f\\u0394\\u039f\\u03a7\\u039f\\u03a3-\\u03a0\\u0397\\u0393\\u0397_003-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"Unnamed Road, Limnos 814 01, Greece\",\"%_wpgmp_location_city%\":\"Limnos\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"Greece\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"8\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.9414\",\"%_wpgmp_metabox_longitude%\":\"25.2853\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2876\",\"%_edit_lock%\":\"1657877324:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%b6%cf%89%ce%bf%ce%b4%cf%8c%cf%87%ce%bf%cf%82-%cf%80%ce%b7%ce%b3%ce%ae-%ce%ba%cf%8c%cf%84%cf%83%ce%b9%ce%bd%ce%b1\",\"%wpcf-latitude%\":\"\",\"%wpcf-longtitude%\":\"\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0396\\u03a9\\u039f\\u0394\\u039f\\u03a7\\u039f\\u03a3-\\u03a0\\u0397\\u0393\\u0397_001.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"21918, 21919, 21920, 21921, 21922\",\"%wpcf-code%\":\"\",\"%wpcf-mapicon%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0396\\u03a9\\u039f\\u0394\\u039f\\u03a7\\u039f\\u03a3-\\u03a0\\u0397\\u0393\\u0397_005.jpg, \\u0396\\u03a9\\u039f\\u0394\\u039f\\u03a7\\u039f\\u03a3 \\u03a0\\u0397\\u0393\\u0397_005, \",\"%_et_pb_truncate_post%\":\"<p>The church of Zoodochos Pigi in Kotsina is one of the most interesting churches in Lemnos due to the underground tunnel that leads to the holy water in the heart of the hill. References to the Zoodochos Pigi church can be traced back to the late Byzantine period when the island was under Venetian rule. Then, the church was located within the walls of the Castle of Kotsina, which was an important port on Lemnos at the time. It was initially dedicated to the Virgin Mary, but it is unknown how it eventually came to be dedicated to Zoodochos Pigi (\\u201cLife-giving well\\u201d). The current building of the church was constructed in the 1950s. To access the holy water of the church, visitors must descend approximately 60 steps down a domed tunnel to the center of the hill where there is a room that is below sea level. The Venetian builders of the Castle understood the value of the underground well, and they preserved it, making it accessible even today. Zoodochos Pigi Kotsina celebrates Easter Friday with a large festival in the church courtyard. A female statue may be seen in the courtyard of Zoodochos Pigi Kotsina.<\\\/p>\\n<p>According to history, this is Maroula, the local hero who led her fellow villagers to drive out\\u00a0the Turks who had\\u00a0besieged the Castle in 1478.<\\\/p>\\n\",\"%_et_pb_truncate_post_date%\":\"2024-01-24 09:48:03\",\"%_et_dynamic_cached_shortcodes%\":\"et_pb_section, et_pb_row, et_pb_column, et_pb_text, et_pb_sidebar, et_pb_divider, et_pb_code, et_pb_image, et_pb_social_media_follow, 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><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-evaggelistria-of-moudros\\\/\\\">The Church of Evaggelistria of Moudros<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-evaggelistria-of-moudros\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The Evaggelistria church of Moudros is the second largest medieval church of Lemnos and Moudros and it dates to the early 20th century (1903). It is a large three-aisled basilica with two bell towers between which is a large arch framed with an impressive window. Entrance to the courtyard is through a carved stone gate. [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8745\",\"lng\":\"25.2697\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-evaggelistria-of-moudros\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The Evaggelistria church of Moudros is the second largest medieval church of Lemnos and Moudros and it dates to the early 20th century (1903). It is a large three-aisled basilica with two bell towers between which is a large arch framed with an impressive window. Entrance to the courtyard is through a carved stone gate. [&hellip;]<\\\/p>\\n\",\"post_content\":\"The Evaggelistria church of Moudros is the second largest medieval church of Lemnos and Moudros and it dates to the early 20<sup>th<\\\/sup> century (1903). It is a large three-aisled basilica with two bell towers between which is a large arch framed with an impressive window. Entrance to the courtyard is through a carved stone gate.\\r\\n\\r\\nThe Evaggelistria Moudros church is at the center of the Annunciation of the Virgin Mary celebrations on Lemnos. During the official opening of the church in 1919, the church's epitaph was donated by Admiral Pavlos Kountouriotis, Chief of the General Staff of the Navy who was stationed on Lemnos during the First World War.\\r\\n\\r\\nThe church\\u2019s tale, on the other hand, is sad and tragic. Before Evaggelistria of Moudros was built on the spot there was a small chapel of Agia Marina which belonged to the Mount Athos monastery of Koutloumousiou. However, when the Turkish rulers of Lemnos discovered the corpses of officers in a well, they burnt down the church and the monks with it in order to take revenge for the killings. The two who managed to escape found sanctuary in Mount Athos, where they claimed some of the locals were provocateurs seeking to destroy the small church to seize its property. The abbot of Koutloumoussiou Monastery decided to impose a punishment (curse) on Moudros, which was finally settled in 2001 with great festivities.\",\"post_title\":\"The Church of Evaggelistria of Moudros\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-evaggelistria-of-moudros\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"The Church of Evaggelistria of Moudros\\\" width=\\\"300\\\" height=\\\"160\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0395\\u03a5\\u0391\\u0393\\u0393\\u0395\\u039b\\u0399\\u03a3\\u03a4\\u03a1\\u0399\\u0391-\\u039c\\u039f\\u03a5\\u0394\\u03a1\\u039f\\u03a5_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"8\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.8745\",\"%_wpgmp_metabox_longitude%\":\"25.2697\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2871\",\"%_edit_lock%\":\"1657877792:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%b5%cf%85%ce%b1%ce%b3%ce%b3%ce%b5%ce%bb%ce%af%cf%83%cf%84%cf%81%ce%b9%ce%b1-%ce%bc%ce%bf%cf%8d%ce%b4%cf%81%ce%bf%cf%85\",\"%wpcf-latitude%\":\"\",\"%wpcf-longtitude%\":\"\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0395\\u03a5\\u0391\\u0393\\u0393\\u0395\\u039b\\u0399\\u03a3\\u03a4\\u03a1\\u0399\\u0391-\\u039c\\u039f\\u03a5\\u0394\\u03a1\\u039f\\u03a5_001.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"21960, 21961, 21962\",\"%wpcf-code%\":\"\",\"%wpcf-mapicon%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0395\\u03a5\\u0391\\u0393\\u0393\\u0395\\u039b\\u0399\\u03a3\\u03a4\\u03a1\\u0399\\u0391-\\u039c\\u039f\\u03a5\\u0394\\u03a1\\u039f\\u03a5_003.jpg, \\u0395\\u03a5\\u0391\\u0393\\u0393\\u0395\\u039b\\u0399\\u03a3\\u03a4\\u03a1\\u0399\\u0391 \\u039c\\u039f\\u03a5\\u0394\\u03a1\\u039f\\u03a5_003, \",\"%_et_pb_truncate_post%\":\"<p>The Evaggelistria church of Moudros is the second largest medieval church of Lemnos and Moudros and it dates to the early 20th century (1903). It is a large three-aisled basilica with two bell towers between which is a large arch framed with an impressive window. Entrance to the courtyard is through a carved stone gate.<\\\/p>\\n<p>The Evaggelistria Moudros church is at the center of the Annunciation of the Virgin Mary celebrations on Lemnos. During the official opening of the church in 1919, the church&#8217;s epitaph was donated by Admiral Pavlos Kountouriotis, Chief of the General Staff of the Navy who was stationed on Lemnos during the First World War.<\\\/p>\\n<p>The church\\u2019s tale, on the other hand, is sad and tragic. Before Evaggelistria of Moudros was built on the spot there was a small chapel of Agia Marina which belonged to the Mount Athos monastery of Koutloumousiou. However, when the Turkish rulers of Lemnos discovered the corpses of officers in a well, they burnt down the church and the monks with it in order to take revenge for the killings. 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class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-st-sozon\\\/\\\">The Church of St. Sozon<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-st-sozon\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Since the Middle Ages, the island's most southeastern edge has been guarded by the small church of Saint Sozontas. According to tradition, a shepherd from the nearby town of Fisini discovered the saint's icon there, and no matter how many times he carried it back to the village, the icon would somehow return to the [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8070\",\"lng\":\"25.3630\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-st-sozon\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Since the Middle Ages, the island's most southeastern edge has been guarded by the small church of Saint Sozontas. According to tradition, a shepherd from the nearby town of Fisini discovered the saint's icon there, and no matter how many times he carried it back to the village, the icon would somehow return to the [&hellip;]<\\\/p>\\n\",\"post_content\":\"Since the Middle Ages, the island's most southeastern edge has been guarded by the small church of Saint Sozontas. According to tradition, a shepherd from the nearby town of Fisini discovered the saint's icon there, and no matter how many times he carried it back to the village, the icon would somehow return to the seaside. So the church was built there, next to the holy water, i.e. a well with fresh water. Another legend states that Saint Sozontas once made his own cape into a boat and saved seamen who were drowning at sea.\\r\\n\\r\\nSaint Sozon became the patron saint of Lemnos when the three-day celebration was established in the early twentieth century. According to legend, it was the sailors of Lemnos who helped establish St. Sozon as the patron saint of Lemnos. They claimed that seeing the modest, all-white chapel at the southeast end of the island glowing from away on the sea, they would find the\\u00a0strength to continue, while sailing their boats.\\r\\n\\r\\nThese days, September 7 marks Saint Sozon Day when people make the pilgrimage to this little church, arriving from all over the world to pray and gather in their hometown.\",\"post_title\":\"The Church of St. Sozon\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-st-sozon\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"The Church of St. Sozon\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u0393\\u0399\\u039f\\u03a3-\\u03a3\\u03a9\\u0396\\u03a9\\u039d_002-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"8\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.8070\",\"%_wpgmp_metabox_longitude%\":\"25.3630\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2869\",\"%_edit_lock%\":\"1657878032:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%ac%ce%b3%ce%b9%ce%bf%cf%82-%cf%83%cf%8e%ce%b6%cf%89%ce%bd-2\",\"%wpcf-latitude%\":\"\",\"%wpcf-longtitude%\":\"\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u0393\\u0399\\u039f\\u03a3-\\u03a3\\u03a9\\u0396\\u03a9\\u039d_001.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"22000, 22001, 22002\",\"%wpcf-code%\":\"\",\"%wpcf-mapicon%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u0393\\u0399\\u039f\\u03a3-\\u03a3\\u03a9\\u0396\\u03a9\\u039d_003.jpg, \\u0391\\u0393\\u0399\\u039f\\u03a3 \\u03a3\\u03a9\\u0396\\u03a9\\u039d_003, \",\"%_et_pb_truncate_post%\":\"<p>Since the Middle Ages, the island&#8217;s most southeastern edge has been guarded by the small church of Saint Sozontas. According to tradition, a shepherd from the nearby town of Fisini discovered the saint&#8217;s icon there, and no matter how many times he carried it back to the village, the icon would somehow return to the seaside. So the church was built there, next to the holy water, i.e. a well with fresh water. Another legend states that Saint Sozontas once made his own cape into a boat and saved seamen who were drowning at sea.<\\\/p>\\n<p>Saint Sozon became the patron saint of Lemnos when the three-day celebration was established in the early twentieth century. According to legend, it was the sailors of Lemnos who helped establish St. Sozon as the patron saint of Lemnos. 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monuments\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/church_result-small.png\"},\"id\":3684,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/church_result-small.png\",\"name\":\"\\u0398\\u03c1\\u03b7\\u03c3\\u03ba\\u03b5\\u03c5\\u03c4\\u03b9\\u03ba\\u03ac \\u03bc\\u03bd\\u03b7\\u03bc\\u03b5\\u03af\\u03b1\",\"id\":\"8\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"The Church of St. Modestos\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"The Church of St. Modestos\\\" width=\\\"274\\\" height=\\\"300\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/modestos-medium.png\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-st-modestos\\\/\\\">The Church of St. Modestos<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-st-modestos\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>St. Modestos is near the Lemnian settlement of Katalakko, on the island's northern coast. The church was completed in 1856 with the money and labour of the locals, who dedicated it to St. Francis of Assisi, the patron saint of animals. The church of St. Modestos features beautiful wood sculptures from the early twentieth century. [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9637\",\"lng\":\"25.1518\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-st-modestos\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>St. Modestos is near the Lemnian settlement of Katalakko, on the island's northern coast. The church was completed in 1856 with the money and labour of the locals, who dedicated it to St. Francis of Assisi, the patron saint of animals. The church of St. Modestos features beautiful wood sculptures from the early twentieth century. [&hellip;]<\\\/p>\\n\",\"post_content\":\"St. Modestos is near the Lemnian settlement of Katalakko, on the island's northern coast. The church was completed in 1856 with the money and labour of the locals, who dedicated it to St. Francis of Assisi, the patron saint of animals.\\r\\n\\r\\nThe church of St. Modestos features beautiful wood sculptures from the early twentieth century.\\r\\n\\r\\nThe feast of St. Modestos is on December 18, when visitors from all around Lemnos gather in the village. The kehagiades of Lemnos, or the island's cattle farmers, used to flock to St. Modestos at night to watch the festivities. They would make a special \\\"koliva\\\" dish that was combined with animal food after the church service in order for the animals\\u00a0to \\\"receive the blessing\\\" and be healthy as well.\",\"post_title\":\"The Church of St. Modestos\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-st-modestos\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"The Church of St. Modestos\\\" width=\\\"274\\\" height=\\\"300\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/modestos-medium.png\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.9637\",\"%_wpgmp_metabox_longitude%\":\"25.1518\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"8\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2984\",\"%_edit_lock%\":\"1657878226:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%ac%ce%b3%ce%b9%ce%bf%cf%82-%ce%bc%cf%8c%ce%b4%ce%b5%cf%83%cf%84%ce%bf%cf%82\",\"%wpcf-latitude%\":\"\",\"%wpcf-longtitude%\":\"\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"\",\"%_wpcf-image-gallery-sort-order%\":\"22038\",\"%wpcf-code%\":\"\",\"%wpcf-mapicon%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/modestos.png, modestos, \",\"%_et_pb_truncate_post%\":\"<p>St. Modestos is near the Lemnian settlement of Katalakko, on the island&#8217;s northern coast. 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monuments\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/church_result-small.png\"},\"id\":3686,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/church_result-small.png\",\"name\":\"\\u0398\\u03c1\\u03b7\\u03c3\\u03ba\\u03b5\\u03c5\\u03c4\\u03b9\\u03ba\\u03ac \\u03bc\\u03bd\\u03b7\\u03bc\\u03b5\\u03af\\u03b1\",\"id\":\"8\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"The Church of St. Ioannis Prodromos of Kontia\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"The Church of St. Ioannis Prodromos of Kontia\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u0393\\u0399\\u039f\\u03a3-\\u0399\\u03a9\\u0391\\u039d\\u039d\\u0397\\u03a3-\\u03a0\\u03a1\\u039f\\u0394\\u03a1\\u039f\\u039c\\u039f\\u03a3-\\u039a\\u039f\\u039d\\u03a4\\u0399\\u0391\\u03a3_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-st-ioannis-prodromos-of-kontia\\\/\\\">The Church of St. Ioannis Prodromos of Kontia<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-st-ioannis-prodromos-of-kontia\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The oldest church in this Lemnos settlement is St. Ioannis Prodromos of Kontia. It was built in the 16th century and is fortified with loopholes and cannons to withstand pirate invasions of the time. The modest church's old icons are an attraction for visitors who have been enjoying the church of St. Ioannis Prodromos of [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.8633\",\"lng\":\"25.1482\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-st-ioannis-prodromos-of-kontia\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The oldest church in this Lemnos settlement is St. Ioannis Prodromos of Kontia. It was built in the 16th century and is fortified with loopholes and cannons to withstand pirate invasions of the time. The modest church's old icons are an attraction for visitors who have been enjoying the church of St. Ioannis Prodromos of [&hellip;]<\\\/p>\\n\",\"post_content\":\"The oldest church in this Lemnos settlement is St. Ioannis Prodromos of Kontia. It was built in the 16<sup>th<\\\/sup> century and is fortified with loopholes and cannons to withstand pirate invasions of the time.\\r\\n\\r\\nThe modest church's old icons are an attraction for visitors who have been enjoying the church of St. Ioannis Prodromos of Kontias as an ecclesiastical museum since the 1970s.\\r\\n\\r\\nThe church is not the only old historic structure in the settlement; the parish church, dedicated to St. Dimitrios, was completed in 1867.\",\"post_title\":\"The Church of St. Ioannis Prodromos of Kontia\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-st-ioannis-prodromos-of-kontia\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"The Church of St. Ioannis Prodromos of Kontia\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u0393\\u0399\\u039f\\u03a3-\\u0399\\u03a9\\u0391\\u039d\\u039d\\u0397\\u03a3-\\u03a0\\u03a1\\u039f\\u0394\\u03a1\\u039f\\u039c\\u039f\\u03a3-\\u039a\\u039f\\u039d\\u03a4\\u0399\\u0391\\u03a3_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"8\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.8633\",\"%_wpgmp_metabox_longitude%\":\"25.1482\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2866\",\"%_edit_lock%\":\"1657878601:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%ac%ce%b3%ce%b9%ce%bf%cf%82-%ce%b9%cf%89%ce%ac%ce%bd%ce%bd%ce%b7%cf%82-%cf%80%cf%81%cf%8c%ce%b4%cf%81%ce%bf%ce%bc%ce%bf%cf%82-%ce%ba%ce%bf%ce%bd%cf%84%ce%b9%ce%ac\",\"%wpcf-latitude%\":\"\",\"%wpcf-longtitude%\":\"\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u0393\\u0399\\u039f\\u03a3-\\u0399\\u03a9\\u0391\\u039d\\u039d\\u0397\\u03a3-\\u03a0\\u03a1\\u039f\\u0394\\u03a1\\u039f\\u039c\\u039f\\u03a3-\\u039a\\u039f\\u039d\\u03a4\\u0399\\u0391\\u03a3_001.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"22075, 22076\",\"%wpcf-code%\":\"\",\"%wpcf-mapicon%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u0393\\u0399\\u039f\\u03a3-\\u0399\\u03a9\\u0391\\u039d\\u039d\\u0397\\u03a3-\\u03a0\\u03a1\\u039f\\u0394\\u03a1\\u039f\\u039c\\u039f\\u03a3-\\u039a\\u039f\\u039d\\u03a4\\u0399\\u0391\\u03a3_002.jpg, \\u0391\\u0393\\u0399\\u039f\\u03a3 \\u0399\\u03a9\\u0391\\u039d\\u039d\\u0397\\u03a3 \\u03a0\\u03a1\\u039f\\u0394\\u03a1\\u039f\\u039c\\u039f\\u03a3 \\u039a\\u039f\\u039d\\u03a4\\u0399\\u0391\\u03a3_002, \",\"%_et_pb_truncate_post%\":\"<p>The oldest church in this Lemnos settlement is St. Ioannis Prodromos of Kontia. It was built in the 16th century and is fortified with loopholes and cannons to withstand pirate invasions of the time.<\\\/p>\\n<p>The modest church&#8217;s old icons are an attraction for visitors who have been enjoying the church of St. Ioannis Prodromos of Kontias as an ecclesiastical museum since the 1970s.<\\\/p>\\n<p>The church is not the only old historic structure in the settlement; the parish church, dedicated to St. Dimitrios, was completed in 1867.<\\\/p>\\n\",\"%_et_pb_truncate_post_date%\":\"2023-08-19 12:25:10\",\"taxonomy=point_category\":\"Religious monuments\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/church_result-small.png\"},\"id\":3688,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/church_result-small.png\",\"name\":\"\\u0398\\u03c1\\u03b7\\u03c3\\u03ba\\u03b5\\u03c5\\u03c4\\u03b9\\u03ba\\u03ac \\u03bc\\u03bd\\u03b7\\u03bc\\u03b5\\u03af\\u03b1\",\"id\":\"8\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"The Church of St. Georgios Repanidiou\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"The Church of St. Georgios Repanidiou\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u0393\\u0399\\u039f\\u03a3-\\u0393\\u0395\\u03a9\\u03a1\\u0393\\u0399\\u039f\\u03a3-\\u03a1\\u0395\\u03a0\\u0391\\u039d\\u0399\\u0394\\u0399\\u039f\\u03a5_002-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-st-georgios-repanidiou\\\/\\\">The Church of St. Georgios Repanidiou<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-st-georgios-repanidiou\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Saint Georgios Repanidiou in Lemnos is an impressive church that has been kept precisely as it was when it was originally built in the middle of the 18th century as the local cemetery church. According to the findings of the church's conservators, St. Georgios Repanidiou was built in the middle of the 18th century (in [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9230\",\"lng\":\"25.3005\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-st-georgios-repanidiou\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Saint Georgios Repanidiou in Lemnos is an impressive church that has been kept precisely as it was when it was originally built in the middle of the 18th century as the local cemetery church. According to the findings of the church's conservators, St. Georgios Repanidiou was built in the middle of the 18th century (in [&hellip;]<\\\/p>\\n\",\"post_content\":\"Saint Georgios Repanidiou in Lemnos is an impressive church that has been kept precisely as it was when it was originally built in the middle of the 18th century as the local cemetery church.\\r\\n\\r\\nAccording to the findings of the church's conservators, St. Georgios Repanidiou was built in the middle of the 18<sup>th<\\\/sup> century (in 1860), as it is a three-aisled post-Byzantine Basilica with neoclassical characteristics, most typical of that time on Lemnos. Its wood-carved iconostasis is stunning, as are its arches with floral depictions on the columns. The church's icons are brightly coloured and described as magnificent examples of post-Byzantine design. St. Georgios Repanidiou has remained unaltered throughout the twentieth century, since the locals decided to build a new church directly next to it in 1928, without replacing the old one.\\r\\n\\r\\nThe recent completion of conservation work at St. Georgios Repanidiou has now provided devout believers and admirers of ecclesiastical art with a monument of great aesthetic significance. The uncovered colourful ceiling, as well as the cared for antiquities, are attracting an increasing number of tourists.\",\"post_title\":\"The Church of St. Georgios Repanidiou\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-st-georgios-repanidiou\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"The Church of St. Georgios Repanidiou\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u0393\\u0399\\u039f\\u03a3-\\u0393\\u0395\\u03a9\\u03a1\\u0393\\u0399\\u039f\\u03a3-\\u03a1\\u0395\\u03a0\\u0391\\u039d\\u0399\\u0394\\u0399\\u039f\\u03a5_002-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"8\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.9230\",\"%_wpgmp_metabox_longitude%\":\"25.3005\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2865\",\"%_edit_lock%\":\"1657878806:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%ac%ce%b3%ce%b9%ce%bf%cf%82-%ce%b3%ce%b5%cf%8e%cf%81%ce%b3%ce%b9%ce%bf%cf%82-%cf%81%ce%b5%cf%80%ce%b1%ce%bd%ce%b9%ce%b4%ce%af%ce%bf%cf%85\",\"%wpcf-latitude%\":\"\",\"%wpcf-longtitude%\":\"\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u0393\\u0399\\u039f\\u03a3-\\u0393\\u0395\\u03a9\\u03a1\\u0393\\u0399\\u039f\\u03a3-\\u03a1\\u0395\\u03a0\\u0391\\u039d\\u0399\\u0394\\u0399\\u039f\\u03a5_001.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"22113, 22114\",\"%wpcf-code%\":\"\",\"%wpcf-mapicon%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u0393\\u0399\\u039f\\u03a3-\\u0393\\u0395\\u03a9\\u03a1\\u0393\\u0399\\u039f\\u03a3-\\u03a1\\u0395\\u03a0\\u0391\\u039d\\u0399\\u0394\\u0399\\u039f\\u03a5_002.jpg, \\u0391\\u0393\\u0399\\u039f\\u03a3 \\u0393\\u0395\\u03a9\\u03a1\\u0393\\u0399\\u039f\\u03a3 \\u03a1\\u0395\\u03a0\\u0391\\u039d\\u0399\\u0394\\u0399\\u039f\\u03a5_002, \",\"%_et_pb_truncate_post%\":\"<p>Saint Georgios Repanidiou in Lemnos is an impressive church that has been kept precisely as it was when it was originally built in the middle of the 18th century as the local cemetery church.<\\\/p>\\n<p>According to the findings of the church&#8217;s conservators, St. Georgios Repanidiou was built in the middle of the 18th century (in 1860), as it is a three-aisled post-Byzantine Basilica with neoclassical characteristics, most typical of that time on Lemnos. Its wood-carved iconostasis is stunning, as are its arches with floral depictions on the columns. The church&#8217;s icons are brightly coloured and described as magnificent examples of post-Byzantine design. St. Georgios Repanidiou has remained unaltered throughout the twentieth century, since the locals decided to build a new church directly next to it in 1928, without replacing the old one.<\\\/p>\\n<p>The recent completion of conservation work at St. Georgios Repanidiou has now provided devout believers and admirers of ecclesiastical art with a monument of great aesthetic significance. 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monuments\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/church_result-small.png\"},\"id\":3689,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/church_result-small.png\",\"name\":\"\\u0398\\u03c1\\u03b7\\u03c3\\u03ba\\u03b5\\u03c5\\u03c4\\u03b9\\u03ba\\u03ac \\u03bc\\u03bd\\u03b7\\u03bc\\u03b5\\u03af\\u03b1\",\"id\":\"8\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"The Church of Saint Georgios Atsikis\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"The Church of Saint Georgios Atsikis\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u0393\\u0399\\u039f\\u03a3-\\u0393\\u0395\\u03a9\\u03a1\\u0393\\u0399\\u039f\\u03a3-\\u0391\\u03a4\\u03a3\\u0399\\u039a\\u0397\\u03a3_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-saint-georgios-atsikis\\\/\\\">The Church of Saint Georgios Atsikis<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-saint-georgios-atsikis\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The parish church of Atsiki on the Greek island of Lemnos is dedicated to St. Georgios and overlooks the village. Completed in 1868, St. Georgios Atsikis is a three-aisled basilica with six distinctive apertures in the exonarthex and eight multifunctional windows on the facade, as well as neoclassical elements, Corinthian pillars, and Russian-style paintings. The [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9458\",\"lng\":\"25.2244\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-saint-georgios-atsikis\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The parish church of Atsiki on the Greek island of Lemnos is dedicated to St. Georgios and overlooks the village. Completed in 1868, St. Georgios Atsikis is a three-aisled basilica with six distinctive apertures in the exonarthex and eight multifunctional windows on the facade, as well as neoclassical elements, Corinthian pillars, and Russian-style paintings. The [&hellip;]<\\\/p>\\n\",\"post_content\":\"The parish church of Atsiki on the Greek island of Lemnos is dedicated to St. Georgios and overlooks the village. Completed in 1868, St. Georgios Atsikis is a three-aisled basilica with six distinctive apertures in the exonarthex and eight multifunctional windows on the facade, as well as neoclassical elements, Corinthian pillars, and Russian-style paintings.\\r\\n\\r\\nThe Church of St. Georgios Atsikis is well-known across Lemnos for having the most beautiful bell tower on the island. It was constructed in 1928 using funds provided by the Atsikians Association of New York. The sculptor Giannis Fotiadis from Samsun built this remarkable bell tower out of Romano stone. The bell tower is 5x5 meters tall and is adorned with intricately carved capitals. Initially, an equally remarkable bell from Russia weighing 400 kg was set on the bell tower, but its ring did not only resound in Atsiki but also in the surrounding villages, forcing the residents of Atsiki to lessen it a few years later.\",\"post_title\":\"The Church of Saint Georgios Atsikis\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/the-church-of-saint-georgios-atsikis\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"The Church of Saint Georgios Atsikis\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u0393\\u0399\\u039f\\u03a3-\\u0393\\u0395\\u03a9\\u03a1\\u0393\\u0399\\u039f\\u03a3-\\u0391\\u03a4\\u03a3\\u0399\\u039a\\u0397\\u03a3_001-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"8\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%_wpgmp_metabox_latitude%\":\"39.9458\",\"%_wpgmp_metabox_longitude%\":\"25.2244\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2862\",\"%_edit_lock%\":\"1657879190:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%ac%ce%b3%ce%b9%ce%bf%cf%82-%ce%b3%ce%b5%cf%8e%cf%81%ce%b3%ce%b9%ce%bf%cf%82-%ce%b1%cf%84%cf%83%ce%b9%ce%ba%ce%ae%cf%82\",\"%wpcf-latitude%\":\"\",\"%wpcf-longtitude%\":\"\",\"%wpcf-location%\":\"\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u0393\\u0399\\u039f\\u03a3-\\u0393\\u0395\\u03a9\\u03a1\\u0393\\u0399\\u039f\\u03a3-\\u0391\\u03a4\\u03a3\\u0399\\u039a\\u0397\\u03a3_003.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"22152, 22153, 22154\",\"%wpcf-code%\":\"\",\"%wpcf-mapicon%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/\\u0391\\u0393\\u0399\\u039f\\u03a3-\\u0393\\u0395\\u03a9\\u03a1\\u0393\\u0399\\u039f\\u03a3-\\u0391\\u03a4\\u03a3\\u0399\\u039a\\u0397\\u03a3_002.jpg, \\u0391\\u0393\\u0399\\u039f\\u03a3 \\u0393\\u0395\\u03a9\\u03a1\\u0393\\u0399\\u039f\\u03a3 \\u0391\\u03a4\\u03a3\\u0399\\u039a\\u0397\\u03a3_002, \",\"%_et_pb_truncate_post%\":\"<p>The parish church of Atsiki on the Greek island of Lemnos is dedicated to St. Georgios and overlooks the village. Completed in 1868, St. Georgios Atsikis is a three-aisled basilica with six distinctive apertures in the exonarthex and eight multifunctional windows on the facade, as well as neoclassical elements, Corinthian pillars, and Russian-style paintings.<\\\/p>\\n<p>The Church of St. Georgios Atsikis is well-known across Lemnos for having the most beautiful bell tower on the island. It was constructed in 1928 using funds provided by the Atsikians Association of New York. The sculptor Giannis Fotiadis from Samsun built this remarkable bell tower out of Romano stone. The bell tower is 5&#215;5 meters tall and is adorned with intricately carved capitals. Initially, an equally remarkable bell from Russia weighing 400 kg was set on the bell tower, but its ring did not only resound in Atsiki but also in the surrounding villages, forcing the residents of Atsiki to lessen it a few years later.<\\\/p>\\n\",\"%_et_pb_truncate_post_date%\":\"2023-08-19 12:25:10\",\"%_et_dynamic_cached_shortcodes%\":\"et_pb_section, et_pb_row, et_pb_column, et_pb_text, et_pb_sidebar, et_pb_divider, et_pb_code, et_pb_image, et_pb_social_media_follow, 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monuments\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/church_result-small.png\"},\"id\":3691,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/church_result-small.png\",\"name\":\"\\u0398\\u03c1\\u03b7\\u03c3\\u03ba\\u03b5\\u03c5\\u03c4\\u03b9\\u03ba\\u03ac \\u03bc\\u03bd\\u03b7\\u03bc\\u03b5\\u03af\\u03b1\",\"id\":\"8\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Aliki (Salt pan) Lake\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Aliki (Salt pan) Lake\\\" width=\\\"300\\\" height=\\\"209\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/38-\\u0391\\u03bb\\u03c5\\u03ba\\u03ae-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/aliki-salt-pan-lake\\\/\\\">Aliki (Salt pan) Lake<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/aliki-salt-pan-lake\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Spanning over 6000 acres, Aliki Lake is located on the northeastern side of Lemnos near the settlement of Kontopouli. The lake is a shallow coastal lagoon filled with water in the winter period and a salt flat in the summer period when it dries. The lake is protected from the marine environment by a 2.5 [&hellip;]<\\\/p>\\n\",\"address\":\"W9RH+VR \\u039c\\u03bf\\u03cd\\u03b4\\u03c1\\u03bf\\u03c2, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.94513282061214\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.37438696289061\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/aliki-salt-pan-lake\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Spanning over 6000 acres, Aliki Lake is located on the northeastern side of Lemnos near the settlement of Kontopouli. The lake is a shallow coastal lagoon filled with water in the winter period and a salt flat in the summer period when it dries. The lake is protected from the marine environment by a 2.5 [&hellip;]<\\\/p>\\n\",\"post_content\":\"Spanning over 6000 acres, Aliki Lake is located on the northeastern side of Lemnos near the settlement of Kontopouli.\\r\\n\\r\\nThe lake is a shallow coastal lagoon filled with water in the winter period and a salt flat in the summer period when it dries.\\r\\n\\r\\nThe lake is protected from the marine environment by a 2.5 km long 100-350 meter wide sandy corridor that acts as a natural dam. The sandy \\\"dam\\\" running parallel to the beach is a coastal geoform occurring mostly on coasts with generally flat landscapes.\\r\\n\\r\\nThe shallow bay began to be separated from\\u00a0the sea 2,900\\u20131,130 years ago today, resulting in the formation of an open lagoon. The creation of the coastal sandy dam was aided by an increase in the rate of sedimentation and a decrease in the rate of sea level rise. The salt lagoon area was a shallow sea bay, sometimes closed, with less influence from the sea, exhibiting lagoon characteristics, and sometimes open, with a stronger sea influence (Sidiropoulou M., 2016).\\r\\n\\r\\nSand dunes develop south of the sandy \\\"dam\\\" and are composed of materials generated from the erosion of molassic formations in the region.\\r\\n\\r\\nAliki is the only natural saltwater lake covering such a large area that has not faced human interference. The region is part of the Natura 2000 network of protected areas. A huge variety of rare and endangered species, including the kestrel and Lanner falcon, use the salt flat for rest, feeding, and breeding.\",\"post_title\":\"Aliki (Salt pan) Lake\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/aliki-salt-pan-lake\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Aliki (Salt pan) Lake\\\" width=\\\"300\\\" height=\\\"209\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/38-\\u0391\\u03bb\\u03c5\\u03ba\\u03ae-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.94513\",\"%wpcf-longtitude%\":\"25.37438\",\"%wpcf-location%\":\"\\u0391\\u03bb\\u03c5\\u03ba\\u03ae\",\"%_wpgmp_metabox_latitude%\":\"39.94513282061214\",\"%_wpgmp_metabox_longitude%\":\"25.37438696289061\",\"%_wpgmp_location_address%\":\"W9RH+VR \\u039c\\u03bf\\u03cd\\u03b4\\u03c1\\u03bf\\u03c2, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"%_wpgmp_location_city%\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:2:{i:0;s:1:\\\"6\\\";i:1;s:2:\\\"15\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/waters.png\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2744\",\"%_edit_lock%\":\"1657098592:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%b1%ce%bb%cf%85%ce%ba%ce%ae\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/38-\\u0391\\u03bb\\u03c5\\u03ba\\u03ae.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20679\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/38-\\u0391\\u03bb\\u03c5\\u03ba\\u03ae.jpg, 38-\\u0391\\u03bb\\u03c5\\u03ba\\u03ae, \",\"%_et_pb_truncate_post%\":\"<p>Spanning over 6000 acres, Aliki Lake is located on the northeastern side of Lemnos near the settlement of Kontopouli.<\\\/p>\\n<p>The lake is a shallow coastal lagoon filled with water in the winter period and a salt flat in the summer period when it dries.<\\\/p>\\n<p>The lake is protected from the marine environment by a 2.5 km long 100-350 meter wide sandy corridor that acts as a natural dam. The sandy &#8220;dam&#8221; running parallel to the beach is a coastal geoform occurring mostly on coasts with generally flat landscapes.<\\\/p>\\n<p>The shallow bay began to be separated from\\u00a0the sea 2,900\\u20131,130 years ago today, resulting in the formation of an open lagoon. The creation of the coastal sandy dam was aided by an increase in the rate of sedimentation and a decrease in the rate of sea level rise. The salt lagoon area was a shallow sea bay, sometimes closed, with less influence from the sea, exhibiting lagoon characteristics, and sometimes open, with a stronger sea influence (Sidiropoulou M., 2016).<\\\/p>\\n<p>Sand dunes develop south of the sandy &#8220;dam&#8221; and are composed of materials generated from the erosion of molassic formations in the region.<\\\/p>\\n<p>Aliki is the only natural saltwater lake covering such a large area that has not faced human interference. The region is part of the Natura 2000 network of protected areas. 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systems\"},\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/apothesis_sm-small.png\"},\"id\":3548,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/waters_result-small.png\",\"name\":\"\\u03a5\\u03b4\\u03b1\\u03c4\\u03b9\\u03ba\\u03ac \\u03c3\\u03c5\\u03c3\\u03c4\\u03ae\\u03bc\\u03b1\\u03c4\\u03b1\",\"id\":\"6\",\"type\":\"category\"},{\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/apothesis_sm-small.png\",\"name\":\"\\u0391\\u03b9\\u03bf\\u03bb\\u03b9\\u03ba\\u03bf\\u03af\",\"id\":\"15\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Gomati Sand Dunes\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Gomati Sand Dunes\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/21-\\u0391\\u03bc\\u03bc\\u03bf\\u03b8\\u03af\\u03bd\\u03b5\\u03c2-\\u0393\\u03bf\\u03bc\\u03ac\\u03c4\\u03b92-scaled-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/gomati-sand-dunes\\\/\\\">Gomati Sand Dunes<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/gomati-sand-dunes\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The Gomati Sand dunes can be found at Gomati, near the settlement of Katalakkos on the northern coast of Lemnos. The sand dunes are large and imposing hills that stand tall in the surrounding landscape. Created by the deposition of sand, these dunes resemble a small desert covering an area of around 70 acres. The [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.991\",\"lng\":\"25.131\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/gomati-sand-dunes\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The Gomati Sand dunes can be found at Gomati, near the settlement of Katalakkos on the northern coast of Lemnos. The sand dunes are large and imposing hills that stand tall in the surrounding landscape. Created by the deposition of sand, these dunes resemble a small desert covering an area of around 70 acres. The [&hellip;]<\\\/p>\\n\",\"post_content\":\"<div class=\\\"sections__field-body\\\">\\r\\n\\r\\nThe Gomati Sand dunes can be found at Gomati, near the settlement of Katalakkos on the northern coast of Lemnos. The sand dunes are large and imposing hills that stand tall in the surrounding landscape. Created by the deposition of sand, these dunes resemble a small desert covering an area of around 70 acres.\\r\\n\\r\\nThe strong NE winds in the area contribute to their creation by transporting and depositing the erosion materials from the surrounding tertiary sedimentary rocks.\\r\\n\\r\\nThe presence of vegetation is crucial to the formation of sand dunes because it actively helps sand retention and protection from further wind erosion.\\r\\n\\r\\n<\\\/div>\",\"post_title\":\"Gomati Sand Dunes\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/gomati-sand-dunes\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Gomati Sand Dunes\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/21-\\u0391\\u03bc\\u03bc\\u03bf\\u03b8\\u03af\\u03bd\\u03b5\\u03c2-\\u0393\\u03bf\\u03bc\\u03ac\\u03c4\\u03b92-scaled-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.991\",\"%wpcf-longtitude%\":\"25.131\",\"%wpcf-location%\":\"\\u0393\\u03bf\\u03bc\\u03ac\\u03c4\\u03b9\",\"%_wpgmp_metabox_latitude%\":\"39.991\",\"%_wpgmp_metabox_longitude%\":\"25.131\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"15\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/apothesis.png\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"3046\",\"%_edit_lock%\":\"1673610567:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%b1%ce%bc%ce%bc%ce%bf%ce%b8%ce%af%ce%bd%ce%b5%cf%82-%ce%b3%ce%bf%ce%bc%ce%ac%cf%84%ce%b9\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/21-\\u0391\\u03bc\\u03bc\\u03bf\\u03b8\\u03af\\u03bd\\u03b5\\u03c2-\\u0393\\u03bf\\u03bc\\u03ac\\u03c4\\u03b92.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20778, 20779, 20780, 20781\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/21-\\u0391\\u03bc\\u03bc\\u03bf\\u03b8\\u03af\\u03bd\\u03b5\\u03c2-\\u0393\\u03bf\\u03bc\\u03ac\\u03c4\\u03b9-4-scaled.jpg, DCIM100MEDIADJI_0119.JPG, DCIM100MEDIADJI_0119.JPG\",\"%_et_pb_truncate_post%\":\"<p>The Gomati Sand dunes can be found at Gomati, near the settlement of Katalakkos on the northern coast of Lemnos. The sand dunes are large and imposing hills that stand tall in the surrounding landscape. 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class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/varos-petrified-tree-trunk\\\/\\\">Varos Petrified Tree Trunk<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/varos-petrified-tree-trunk\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>An impressive petrified tree trunk of an angiosperm tree can be found lying on its side in the fossil-rich area located outside the village of Varos. The biggest part of the fossilized trunk was found covered with soil, while its lower side was discovered in pyroclastic rocks. With the completion of the first phase of [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.930\",\"lng\":\"25.257\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/varos-petrified-tree-trunk\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>An impressive petrified tree trunk of an angiosperm tree can be found lying on its side in the fossil-rich area located outside the village of Varos. The biggest part of the fossilized trunk was found covered with soil, while its lower side was discovered in pyroclastic rocks. With the completion of the first phase of [&hellip;]<\\\/p>\\n\",\"post_content\":\"An impressive petrified tree trunk of an angiosperm tree can be found lying on its side in the fossil-rich area located outside the village of Varos.\\r\\n\\r\\nThe biggest part of the fossilized trunk was found covered with soil, while its lower side was discovered in pyroclastic rocks. With the completion of the first phase of excavations by the Natural History Museum of the Lesvos Petrified Forest, it was revealed that the trunk\\u2019s diameter exceeds 1 m and its length is greater than 7m.\\r\\n\\r\\nMaterials of volcanic origin, such as volcanic ash and pyroclastic flows of massive volcanic eruptions, swept over and covered the petrified forest of Lemnos approximately 22.3 million years ago. The massive trunk of the Varos angiosperm tree was snapped and dragged to its present location by the pyroclastic flows. The thick layer of volcanic material isolated the trunk from the external conditions, creating an ideal environment for its fossilization.\\r\\n\\r\\nThus, the morphological characteristics of the tree such as the stunning knots and the internal wood structure were preserved in perfect condition. 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With the completion of the first phase of excavations by the Natural History Museum of the Lesvos Petrified Forest, it was revealed that the trunk\\u2019s diameter exceeds 1 m and its length is greater than 7m.<\\\/p>\\n<p>Materials of volcanic origin, such as volcanic ash and pyroclastic flows of massive volcanic eruptions, swept over and covered the petrified forest of Lemnos approximately 22.3 million years ago. The massive trunk of the Varos angiosperm tree was snapped and dragged to its present location by the pyroclastic flows. The thick layer of volcanic material isolated the trunk from the external conditions, creating an ideal environment for its fossilization.<\\\/p>\\n<p>Thus, the morphological characteristics of the tree such as the stunning knots and the internal wood structure were preserved in perfect condition. 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class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/vougiatzidika-ichnofossils\\\/\\\">Vougiatzidika Ichnofossils<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/vougiatzidika-ichnofossils\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The sandstone layers of Lemnos\\u2019 molassic formations include a big variety of ichnofossils known as graphoglyptids, which often appear towards the base sandstone 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The ichnfossils discovered on Lemnos belong to the Crusiana, Zoophycos, Scolithos, and Nereites groups. The fossils are characterized by the final group of Nereites, confirming that the Lemnos sandstone sediments formed [&hellip;]<\\\/p>\\n\",\"address\":\"X6RV+Q5 \\u0391\\u03c4\\u03c3\\u03b9\\u03ba\\u03ae, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.99197524255613\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.242924930175786\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/vougiatzidika-ichnofossils\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The sandstone layers of Lemnos\\u2019 molassic formations include a big variety of ichnofossils known as graphoglyptids, which often appear towards the base sandstone layers. The ichnfossils discovered on Lemnos belong to the Crusiana, Zoophycos, Scolithos, and Nereites groups. The fossils are characterized by the final group of Nereites, confirming that the Lemnos sandstone sediments formed [&hellip;]<\\\/p>\\n\",\"post_content\":\"The sandstone layers of Lemnos\\u2019 molassic formations include a big variety of ichnofossils known as graphoglyptids, which often appear towards the base sandstone layers.\\r\\n\\r\\nThe ichnfossils discovered on Lemnos belong to the Crusiana, Zoophycos, Scolithos, and Nereites groups.\\r\\n\\r\\nThe fossils are characterized by the final group of Nereites, confirming that the Lemnos sandstone sediments formed in the marine environment as deposits of submerged debris in oxygen-rich circumstances.\",\"post_title\":\"Vougiatzidika Ichnofossils\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/vougiatzidika-ichnofossils\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Vougiatzidika Ichnofossils\\\" width=\\\"300\\\" height=\\\"192\\\" 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sites\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/fossil_result-small.png\"},\"id\":3554,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/fossil_result-small.png\",\"name\":\"\\u0391\\u03c0\\u03bf\\u03bb\\u03b9\\u03b8\\u03c9\\u03bc\\u03b1\\u03c4\\u03bf\\u03c6\\u03cc\\u03c1\\u03b5\\u03c2 \\u0398\\u03ad\\u03c3\\u03b5\\u03b9\\u03c2\",\"id\":\"1\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Chavouli Moudros Fossil Site\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Chavouli Moudros Fossil Site\\\" width=\\\"300\\\" height=\\\"226\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/44-\\u0391\\u03c0\\u03bf\\u03bb\\u03b9\\u03b8\\u03c9\\u03bc\\u03b1\\u03c4\\u03bf\\u03c6\\u03cc\\u03c1\\u03bf\\u03c2-\\u03b8\\u03ad\\u03c3\\u03b7-\\u03a7\\u03b1\\u03b2\\u03bf\\u03cd\\u03bb\\u03b9-\\u039c\\u03bf\\u03cd\\u03b4\\u03c1\\u03bf\\u03c5-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/chavouli-moudros-fossil-site\\\/\\\">Chavouli Moudros Fossil Site<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/chavouli-moudros-fossil-site\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>On the SE peninsula of Lemnos, important plant fossils representing the forest flora of the area 23 million years ago have been found at the Chavouli Moudros site. Among these fossils, an impressive standing fossilized trunk was found. While most of it is buried in pyroclastic rocks, the visible part of this trunk stands 50 [&hellip;]<\\\/p>\\n\",\"address\":\"V73P+6F \\u039c\\u03bf\\u03cd\\u03b4\\u03c1\\u03bf\\u03c2, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.853194682890155\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.286249343872054\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/chavouli-moudros-fossil-site\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>On the SE peninsula of Lemnos, important plant fossils representing the forest flora of the area 23 million years ago have been found at the Chavouli Moudros site. Among these fossils, an impressive standing fossilized trunk was found. While most of it is buried in pyroclastic rocks, the visible part of this trunk stands 50 [&hellip;]<\\\/p>\\n\",\"post_content\":\"On the SE peninsula of Lemnos, important plant fossils representing the forest flora of the area 23 million years ago have been found at the Chavouli Moudros site.\\r\\n\\r\\nAmong these fossils, an impressive standing fossilized trunk was found. While most of it is buried in pyroclastic rocks, the visible part of this trunk stands 50 cm tall.\\r\\n\\r\\nThe products of the volcanic eruptions of Lemnos\\u2019 volcanoes razed and buried the forest that thrived there about 22.3 million years ago. A heavy layer of volcanic debris coated the trunk. These materials surrounded the tree trunk, isolating it and creating excellent conditions for fossilization. The absence of oxygen, along with the presence of hydrothermal solutions, established the ideal environment for silicates to replace organic plant matter molecule by molecule, resulting in the perfect fossilization of wood. As a result, the tree\\u2019s morphological qualities, such as the internal and external structure of the wood, remained in good condition.\\r\\n\\r\\nThe fossilized trunk was brought to the surface by the erosion of the pyroclastic rocks over time.\",\"post_title\":\"Chavouli Moudros Fossil Site\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/chavouli-moudros-fossil-site\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Chavouli Moudros Fossil Site\\\" width=\\\"300\\\" height=\\\"226\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/44-\\u0391\\u03c0\\u03bf\\u03bb\\u03b9\\u03b8\\u03c9\\u03bc\\u03b1\\u03c4\\u03bf\\u03c6\\u03cc\\u03c1\\u03bf\\u03c2-\\u03b8\\u03ad\\u03c3\\u03b7-\\u03a7\\u03b1\\u03b2\\u03bf\\u03cd\\u03bb\\u03b9-\\u039c\\u03bf\\u03cd\\u03b4\\u03c1\\u03bf\\u03c5-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%_wpgmp_metabox_latitude%\":\"39.853194682890155\",\"%_wpgmp_metabox_longitude%\":\"25.286249343872054\",\"%_wpgmp_location_address%\":\"V73P+6F \\u039c\\u03bf\\u03cd\\u03b4\\u03c1\\u03bf\\u03c2, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"%_wpgmp_location_city%\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"1\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%wpcf-latitude%\":\"39.853\",\"%wpcf-longtitude%\":\"25.286\",\"%wpcf-location%\":\"\\u03a0\\u03ad\\u03c4\\u03c1\\u03c9\\u03bc\\u03b1 (\\u03c7\\u03b1\\u03bc\\u03b7\\u03bb\\u03ac)\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/fossil-1.png\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_wpml_location_migration_done%\":\"1\",\"%_wpml_word_count%\":\"{\\\"total\\\":177,\\\"to_translate\\\":{\\\"en\\\":177}}\",\"%_thumbnail_id%\":\"2783\",\"%_edit_lock%\":\"1655204105:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%b1%cf%80%ce%bf%ce%bb%ce%b9%ce%b8%cf%89%ce%bc%ce%b1%cf%84%ce%bf%cf%86%cf%8c%cf%81%ce%bf%cf%82-%ce%b8%ce%ad%cf%83%ce%b7-%cf%87%ce%b1%ce%b2%ce%bf%cf%8d%ce%bb%ce%b9-%ce%bc%ce%bf%cf%8d%ce%b4%cf%81\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/44-\\u0391\\u03c0\\u03bf\\u03bb\\u03b9\\u03b8\\u03c9\\u03bc\\u03b1\\u03c4\\u03bf\\u03c6\\u03cc\\u03c1\\u03bf\\u03c2-\\u03b8\\u03ad\\u03c3\\u03b7-\\u03a7\\u03b1\\u03b2\\u03bf\\u03cd\\u03bb\\u03b9-\\u039c\\u03bf\\u03cd\\u03b4\\u03c1\\u03bf\\u03c5.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"19427\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/44-\\u0391\\u03c0\\u03bf\\u03bb\\u03b9\\u03b8\\u03c9\\u03bc\\u03b1\\u03c4\\u03bf\\u03c6\\u03cc\\u03c1\\u03bf\\u03c2-\\u03b8\\u03ad\\u03c3\\u03b7-\\u03a7\\u03b1\\u03b2\\u03bf\\u03cd\\u03bb\\u03b9-\\u039c\\u03bf\\u03cd\\u03b4\\u03c1\\u03bf\\u03c5.jpg, 44-\\u0391\\u03c0\\u03bf\\u03bb\\u03b9\\u03b8\\u03c9\\u03bc\\u03b1\\u03c4\\u03bf\\u03c6\\u03cc\\u03c1\\u03bf\\u03c2 \\u03b8\\u03ad\\u03c3\\u03b7 \\u03a7\\u03b1\\u03b2\\u03bf\\u03cd\\u03bb\\u03b9 \\u039c\\u03bf\\u03cd\\u03b4\\u03c1\\u03bf\\u03c5, \",\"%_et_pb_truncate_post%\":\"<p>On the SE peninsula of Lemnos, important plant fossils representing the forest flora of the area 23 million years ago have been found at the Chavouli Moudros site.<\\\/p>\\n<p>Among these fossils, an impressive standing fossilized trunk was found. 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sites\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/fossil_result-small.png\"},\"id\":3556,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/fossil_result-small.png\",\"name\":\"\\u0391\\u03c0\\u03bf\\u03bb\\u03b9\\u03b8\\u03c9\\u03bc\\u03b1\\u03c4\\u03bf\\u03c6\\u03cc\\u03c1\\u03b5\\u03c2 \\u0398\\u03ad\\u03c3\\u03b5\\u03b9\\u03c2\",\"id\":\"1\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Roussopouli Information Center\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Roussopouli Information Center\\\" width=\\\"300\\\" height=\\\"220\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/50-\\u039a\\u03ad\\u03bd\\u03c4\\u03c1\\u03bf-\\u03b5\\u03bd\\u03b7\\u03bc\\u03ad\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-\\u03a1\\u03bf\\u03c5\\u03c3\\u03c3\\u03bf\\u03c0\\u03bf\\u03c5\\u03bb\\u03af\\u03bf\\u03c5-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/roussopouli-information-center\\\/\\\">Roussopouli Information Center<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/roussopouli-information-center\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Roussopouli is located near to the east of Moudros settlement. Situated amphitheatrically on the slopes of the Korakas hill, the center is located a short distance from Chortarolimni, one of Lemnos\\u2019 most important wetlands. The Visitor Information Center showcases the geo-history, geo-monuments, and geosites of Lemnos, as well as the natural environment and rural heritage [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.88407\",\"lng\":\"25.309815\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/roussopouli-information-center\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Roussopouli is located near to the east of Moudros settlement. Situated amphitheatrically on the slopes of the Korakas hill, the center is located a short distance from Chortarolimni, one of Lemnos\\u2019 most important wetlands. The Visitor Information Center showcases the geo-history, geo-monuments, and geosites of Lemnos, as well as the natural environment and rural heritage [&hellip;]<\\\/p>\\n\",\"post_content\":\"Roussopouli is located near to the east of Moudros settlement. 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Situated amphitheatrically on the slopes of the Korakas hill, the center is located a short distance from Chortarolimni, one of Lemnos\\u2019 most important wetlands.<\\\/p>\\n<p>The Visitor Information Center showcases the geo-history, geo-monuments, and geosites of Lemnos, as well as the natural environment and rural heritage of the area, particularly as it is housed in the spectacular building of the old school in Roussopouli.<\\\/p>\\n<p>The center is equipped with the latest technology and offers digital applications linked to geo-monuments and geosites of Lemnos island.<\\\/p>\\n\",\"%_et_pb_truncate_post_date%\":\"2023-01-04 04:11:03\",\"%_et_dynamic_cached_shortcodes%\":\"et_pb_section, et_pb_row, et_pb_column, et_pb_text, et_pb_sidebar, et_pb_divider, et_pb_code, et_pb_image, et_pb_social_media_follow, 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sites\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/fossil_result-small.png\"},\"id\":3557,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/fossil_result-small.png\",\"name\":\"\\u0391\\u03c0\\u03bf\\u03bb\\u03b9\\u03b8\\u03c9\\u03bc\\u03b1\\u03c4\\u03bf\\u03c6\\u03cc\\u03c1\\u03b5\\u03c2 \\u0398\\u03ad\\u03c3\\u03b5\\u03b9\\u03c2\",\"id\":\"1\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"St. Pavlos Volcanic Dome\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"St. Pavlos Volcanic Dome\\\" width=\\\"300\\\" height=\\\"208\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/10-\\u0397\\u03c6\\u03b1\\u03b9\\u03c3\\u03c4\\u03b5\\u03b9\\u03b1\\u03ba\\u03cc\\u03c2-\\u03b4\\u03cc\\u03bc\\u03bf\\u03c2-\\u0391\\u03b3\\u03af\\u03bf\\u03c5-\\u03a0\\u03b1\\u03cd\\u03bb\\u03bf\\u03c5-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/st-pavlos-volcanic-dome\\\/\\\">St. Pavlos Volcanic Dome<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/st-pavlos-volcanic-dome\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Near the town of Thanos in SW Lemnos, a highly distinctive volcanic formation stands by the sea. The volcanic dome on the hill of Saint Pavlos is a conical volcanic formation composed of dacitic lava which formed 19.3-18.2 million years ago. The formation of this dome is related to the intense volcanic activity that created [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.845\",\"lng\":\"25.104\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/st-pavlos-volcanic-dome\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Near the town of Thanos in SW Lemnos, a highly distinctive volcanic formation stands by the sea. The volcanic dome on the hill of Saint Pavlos is a conical volcanic formation composed of dacitic lava which formed 19.3-18.2 million years ago. The formation of this dome is related to the intense volcanic activity that created [&hellip;]<\\\/p>\\n\",\"post_content\":\"Near the town of Thanos in SW Lemnos, a highly distinctive volcanic formation stands by the sea. The volcanic dome on the hill of Saint Pavlos is a conical volcanic formation composed of dacitic lava which formed 19.3-18.2 million years ago.\\r\\n\\r\\nThe formation of this dome is related to the intense volcanic activity that created the chain of volcanic domes in southwestern Lemnos. Rising magma with a high potassium and silicon concentration permeated the pre-existing sedimentary and pyroclastic geological formations, causing their uplifting. In some cases, the volcanic material surfaced as thick lava, where it instantly cooled, forming the distinctive volcanic structure which characterizes the area\\u2019s terrain.\",\"post_title\":\"St. Pavlos Volcanic Dome\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/st-pavlos-volcanic-dome\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"St. Pavlos Volcanic Dome\\\" width=\\\"300\\\" height=\\\"208\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/10-\\u0397\\u03c6\\u03b1\\u03b9\\u03c3\\u03c4\\u03b5\\u03b9\\u03b1\\u03ba\\u03cc\\u03c2-\\u03b4\\u03cc\\u03bc\\u03bf\\u03c2-\\u0391\\u03b3\\u03af\\u03bf\\u03c5-\\u03a0\\u03b1\\u03cd\\u03bb\\u03bf\\u03c5-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.845\",\"%wpcf-longtitude%\":\"25.104\",\"%wpcf-location%\":\"\\u0386\\u03b3\\u03b9\\u03bf\\u03c2 \\u03a0\\u03b1\\u03cd\\u03bb\\u03bf\\u03c2\",\"%_wpgmp_metabox_latitude%\":\"39.845\",\"%_wpgmp_metabox_longitude%\":\"25.104\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"4\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/volcanos.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%wpcf-code%\":\"\",\"%_wpml_location_migration_done%\":\"1\",\"%_wpml_word_count%\":\"{\\\"total\\\":127,\\\"to_translate\\\":{\\\"en\\\":127}}\",\"%_thumbnail_id%\":\"2757\",\"%_edit_lock%\":\"1655204960:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%b7%cf%86%ce%b1%ce%b9%cf%83%cf%84%ce%b5%ce%b9%ce%b1%ce%ba%cf%8c%cf%82-%ce%b4%cf%8c%ce%bc%ce%bf%cf%82-%ce%b1%ce%b3%ce%af%ce%bf%cf%85-%cf%80%ce%b1%cf%8d%ce%bb%ce%bf%cf%85\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/10-\\u0397\\u03c6\\u03b1\\u03b9\\u03c3\\u03c4\\u03b5\\u03b9\\u03b1\\u03ba\\u03cc\\u03c2-\\u03b4\\u03cc\\u03bc\\u03bf\\u03c2-\\u0391\\u03b3\\u03af\\u03bf\\u03c5-\\u03a0\\u03b1\\u03cd\\u03bb\\u03bf\\u03c5.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"19499\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/10-\\u0397\\u03c6\\u03b1\\u03b9\\u03c3\\u03c4\\u03b5\\u03b9\\u03b1\\u03ba\\u03cc\\u03c2-\\u03b4\\u03cc\\u03bc\\u03bf\\u03c2-\\u0391\\u03b3\\u03af\\u03bf\\u03c5-\\u03a0\\u03b1\\u03cd\\u03bb\\u03bf\\u03c5.jpg, 10-\\u0397\\u03c6\\u03b1\\u03b9\\u03c3\\u03c4\\u03b5\\u03b9\\u03b1\\u03ba\\u03cc\\u03c2 \\u03b4\\u03cc\\u03bc\\u03bf\\u03c2 \\u0391\\u03b3\\u03af\\u03bf\\u03c5 \\u03a0\\u03b1\\u03cd\\u03bb\\u03bf\\u03c5, \",\"%_et_pb_truncate_post%\":\"<p>Near the town of Thanos in SW Lemnos, a highly distinctive volcanic formation stands by the sea. The volcanic dome on the hill of Saint Pavlos is a conical volcanic formation composed of dacitic lava which formed 19.3-18.2 million years ago.<\\\/p>\\n<p>The formation of this dome is related to the intense volcanic activity that created the chain of volcanic domes in southwestern Lemnos. Rising magma with a high potassium and silicon concentration permeated the pre-existing sedimentary and pyroclastic geological formations, causing their uplifting. 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geosites\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/volcanos_result-small.png\"},\"id\":3558,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/volcanos_result-small.png\",\"name\":\"\\u0397\\u03c6\\u03b1\\u03b9\\u03c3\\u03c4\\u03b5\\u03b9\\u03b1\\u03ba\\u03bf\\u03af\",\"id\":\"4\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Kakavos Volcanic Dyke\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Kakavos Volcanic Dyke\\\" width=\\\"300\\\" height=\\\"144\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/14-\\u0397\\u03c6\\u03b1\\u03b9\\u03c3\\u03c4\\u03b5\\u03b9\\u03b1\\u03ba\\u03ae-\\u03c6\\u03bb\\u03ad\\u03b2\\u03b1-\\u039a\\u03ac\\u03ba\\u03b1\\u03b2\\u03bf\\u03c5-\\u03b9\\u03c3\\u03c4\\u03bf\\u03c3\\u03b5\\u03bb\\u03b9\\u03b4\\u03b1-2-scaled-medium.jpg\\\" class=\\\"wp-post-image  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This characteristic volcanic structure is a set of parallel and nearly vertical lava \\u201cwalls\\u201d that stand upright in the surrounding plain. This volcanic structure was formed by the intrusion of andesitic magma through faults in the crust where it [&hellip;]<\\\/p>\\n\",\"address\":\"V4F2+CV \\u039c\\u03cd\\u03c1\\u03b9\\u03bd\\u03b1, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.87360108165118\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.102158714294447\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kakavos-volcanic-dyke\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The Kakavos Volcanic dyke is located alongside the road that leads to the Kakavos volcanic hill. This characteristic volcanic structure is a set of parallel and nearly vertical lava \\u201cwalls\\u201d that stand upright in the surrounding plain. This volcanic structure was formed by the intrusion of andesitic magma through faults in the crust where it [&hellip;]<\\\/p>\\n\",\"post_content\":\"The Kakavos Volcanic dyke is located alongside the road that leads to the Kakavos volcanic hill. This characteristic volcanic structure is a set of parallel and nearly vertical lava \\u201cwalls\\u201d that stand upright in the surrounding plain.\\r\\n\\r\\nThis volcanic structure was formed by the intrusion of andesitic magma through faults in the crust where it solidified with time, creating the impressive volcanic structure. 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geosites\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/volcanos_result-small.png\"},\"id\":3560,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/volcanos_result-small.png\",\"name\":\"\\u0397\\u03c6\\u03b1\\u03b9\\u03c3\\u03c4\\u03b5\\u03b9\\u03b1\\u03ba\\u03bf\\u03af\",\"id\":\"4\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Profitis Ilias Volcanic Dome\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Profitis Ilias Volcanic Dome\\\" width=\\\"300\\\" height=\\\"215\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/19-\\u03a0\\u03c1\\u03bf\\u03c6\\u03ae\\u03c4\\u03b7\\u03c2-\\u0397\\u03bb\\u03af\\u03b1\\u03c2-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/profitis-ilias-volcanic-dome\\\/\\\">Profitis Ilias Volcanic Dome<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/profitis-ilias-volcanic-dome\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The impressive hill of Profitis Ilias dominating the landscape is one of the most characteristic volcanic structures of Lemnos. Located to the west of the gulf of Moudros, south of the village of Kornos, the hot springs of Therma flow from its foothills. The volcanic dome was formed by the uplifting of the volcanic rocks [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.896\",\"lng\":\"25.129\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/profitis-ilias-volcanic-dome\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The impressive hill of Profitis Ilias dominating the landscape is one of the most characteristic volcanic structures of Lemnos. Located to the west of the gulf of Moudros, south of the village of Kornos, the hot springs of Therma flow from its foothills. The volcanic dome was formed by the uplifting of the volcanic rocks [&hellip;]<\\\/p>\\n\",\"post_content\":\"The impressive hill of Profitis Ilias dominating the landscape is one of the most characteristic volcanic structures of Lemnos. Located to the west of the gulf of Moudros, south of the village of Kornos, the hot springs of Therma flow from its foothills.\\r\\n\\r\\nThe volcanic dome was formed by the uplifting of the volcanic rocks as dacitic lava permeated the crust. The hill of Profitis Ilias belongs to a complex of volcanic structures created 19.3-18.2 million years ago in western Lemnos by magma with a relatively high gas content which permeated and uplifted pre-existing geological formations before it rapidly cooled.\\r\\n\\r\\nAt the highest points of the volcanic dome there are weathering formations called \\u201ctafoni\\u201d, which are fascinating structures caused by erosion of the volcanic rocks.\\r\\n\\r\\nThe towering volcanic hill of Profitis Ilias appears to have been well-known among foreign visitors. There are instances, such as that of the French Ambassador to the Ottoman Empire, Auguste de Choiseul \\u2013 Gouffie (1785), where the volcanic structure is referred to as the Therma Mountain (Mt. de Therma).\",\"post_title\":\"Profitis Ilias Volcanic Dome\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/profitis-ilias-volcanic-dome\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Profitis Ilias Volcanic Dome\\\" width=\\\"300\\\" height=\\\"215\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/19-\\u03a0\\u03c1\\u03bf\\u03c6\\u03ae\\u03c4\\u03b7\\u03c2-\\u0397\\u03bb\\u03af\\u03b1\\u03c2-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.896\",\"%wpcf-longtitude%\":\"25.129\",\"%wpcf-location%\":\"\\u03a0\\u03c1\\u03bf\\u03c6\\u03ae\\u03c4\\u03b7\\u03c2 \\u0397\\u03bb\\u03af\\u03b1\\u03c2\",\"%_wpgmp_metabox_latitude%\":\"39.896\",\"%_wpgmp_metabox_longitude%\":\"25.129\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"4\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/volcanos.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%wpcf-code%\":\"\",\"%_wpml_location_migration_done%\":\"1\",\"%_wpml_word_count%\":\"{\\\"total\\\":181,\\\"to_translate\\\":{\\\"en\\\":181}}\",\"%_thumbnail_id%\":\"2766\",\"%_edit_lock%\":\"1655205339:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%b7%cf%86%ce%b1%ce%b9%cf%83%cf%84%ce%b5%ce%b9%ce%b1%ce%ba%cf%8c%cf%82-%ce%b4%cf%8c%ce%bc%ce%bf%cf%82-%cf%80%cf%81%ce%bf%cf%86%ce%ae%cf%84%ce%b7%cf%82-%ce%b7%ce%bb%ce%af%ce%b1%cf%82\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/19-\\u03a0\\u03c1\\u03bf\\u03c6\\u03ae\\u03c4\\u03b7\\u03c2-\\u0397\\u03bb\\u03af\\u03b1\\u03c2.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"19571\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/19-\\u03a0\\u03c1\\u03bf\\u03c6\\u03ae\\u03c4\\u03b7\\u03c2-\\u0397\\u03bb\\u03af\\u03b1\\u03c2.jpg, 19-\\u03a0\\u03c1\\u03bf\\u03c6\\u03ae\\u03c4\\u03b7\\u03c2 \\u0397\\u03bb\\u03af\\u03b1\\u03c2, \",\"%_et_pb_truncate_post%\":\"<p>The impressive hill of Profitis Ilias dominating the landscape is one of the most characteristic volcanic structures of Lemnos. Located to the west of the gulf of Moudros, south of the village of Kornos, the hot springs of Therma flow from its foothills.<\\\/p>\\n<p>The volcanic dome was formed by the uplifting of the volcanic rocks as dacitic lava permeated the crust. The hill of Profitis Ilias belongs to a complex of volcanic structures created 19.3-18.2 million years ago in western Lemnos by magma with a relatively high gas content which permeated and uplifted pre-existing geological formations before it rapidly cooled.<\\\/p>\\n<p>At the highest points of the volcanic dome there are weathering formations called \\u201ctafoni\\u201d, which are fascinating structures caused by erosion of the volcanic rocks.<\\\/p>\\n<p>The towering volcanic hill of Profitis Ilias appears to have been well-known among foreign visitors. There are instances, such as that of the French Ambassador to the Ottoman Empire, Auguste de Choiseul \\u2013 Gouffie (1785), where the volcanic structure is referred to as the Therma Mountain (Mt. de Therma).<\\\/p>\\n\",\"%_et_pb_truncate_post_date%\":\"2023-01-06 08:46:59\",\"%_et_dynamic_cached_shortcodes%\":\"et_pb_section, et_pb_row, et_pb_column, et_pb_text, et_pb_sidebar, et_pb_divider, et_pb_code, et_pb_image, et_pb_social_media_follow, 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geosites\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/volcanos_result-small.png\"},\"id\":3561,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/volcanos_result-small.png\",\"name\":\"\\u0397\\u03c6\\u03b1\\u03b9\\u03c3\\u03c4\\u03b5\\u03b9\\u03b1\\u03ba\\u03bf\\u03af\",\"id\":\"4\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Palaiokastro Volcanic Dome\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Palaiokastro Volcanic Dome\\\" width=\\\"300\\\" height=\\\"210\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/17-\\u0397\\u03c6\\u03b1\\u03b9\\u03c3\\u03c4\\u03b5\\u03b9\\u03b1\\u03ba\\u03cc\\u03c2-\\u03b4\\u03cc\\u03bc\\u03bf\\u03c2-\\u03a0\\u03b1\\u03bb\\u03b1\\u03b9\\u03cc\\u03ba\\u03b1\\u03c3\\u03c4\\u03c1\\u03bf\\u03c5-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/palaiokastro-volcanic-dome\\\/\\\">Palaiokastro Volcanic Dome<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/palaiokastro-volcanic-dome\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Palaiokastro Volcanic Dome is a characteristic volcanic structure in the western part of Lemnos, visible to the visitor from the parking lot on the road to the chapel of Panagia Kakaviotissa. The scattered hills in the area form a network of volcanic structures that were created 19.3-18.2 million years ago. The permeation of viscous magma [&hellip;]<\\\/p>\\n\",\"address\":\"V4H6+RF \\u039c\\u03cd\\u03c1\\u03b9\\u03bd\\u03b1, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.87919279928601\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.111099701019278\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/palaiokastro-volcanic-dome\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Palaiokastro Volcanic Dome is a characteristic volcanic structure in the western part of Lemnos, visible to the visitor from the parking lot on the road to the chapel of Panagia Kakaviotissa. The scattered hills in the area form a network of volcanic structures that were created 19.3-18.2 million years ago. The permeation of viscous magma [&hellip;]<\\\/p>\\n\",\"post_content\":\"Palaiokastro Volcanic Dome is a characteristic volcanic structure in the western part of Lemnos, visible to the visitor from the parking lot on the road to the chapel of Panagia Kakaviotissa.\\r\\n\\r\\nThe scattered hills in the area form a network of volcanic structures that were created 19.3-18.2 million years ago. The permeation of viscous magma with high gas content caused the uplifting of older sedimentary and volcanic rock. 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geosites\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/volcanos_result-small.png\"},\"id\":3563,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/volcanos_result-small.png\",\"name\":\"\\u0397\\u03c6\\u03b1\\u03b9\\u03c3\\u03c4\\u03b5\\u03b9\\u03b1\\u03ba\\u03bf\\u03af\",\"id\":\"4\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Kakavos Volcanic Domes\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Kakavos Volcanic Domes\\\" width=\\\"300\\\" height=\\\"210\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/15-\\u0397\\u03c6\\u03b1\\u03b9\\u03c3\\u03c4\\u03b5\\u03b9\\u03b1\\u03ba\\u03bf\\u03af-\\u03b4\\u03cc\\u03bc\\u03bf\\u03b9-\\u039a\\u03ac\\u03ba\\u03b1\\u03b2\\u03bf\\u03c5-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kakavos-volcanic-domes\\\/\\\">Kakavos Volcanic Domes<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kakavos-volcanic-domes\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Northeast of the village of Thanos is a chain of conical hills which are the volcanic structures that characterize the unique landscape of southwest Lemnos. These volcanic structures were formed 19.3-18.2 million years ago, when dacitic magma rose to the surface through tectonic discontinuities in the crust, permeating pre-existing sedimentary and volcanic formations. When the [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.870\",\"lng\":\"25.108\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kakavos-volcanic-domes\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Northeast of the village of Thanos is a chain of conical hills which are the volcanic structures that characterize the unique landscape of southwest Lemnos. These volcanic structures were formed 19.3-18.2 million years ago, when dacitic magma rose to the surface through tectonic discontinuities in the crust, permeating pre-existing sedimentary and volcanic formations. When the [&hellip;]<\\\/p>\\n\",\"post_content\":\"Northeast of the village of Thanos is a chain of conical hills which are the volcanic structures that characterize the unique landscape of southwest Lemnos.\\r\\n\\r\\nThese volcanic structures were formed 19.3-18.2 million years ago, when dacitic magma rose to the surface through tectonic discontinuities in the crust, permeating pre-existing sedimentary and volcanic formations. When the viscous magma surfaced, it cooled swiftly, thus forming the characteristic dome structures.\\r\\n\\r\\nThese volcacin domes show intense erosion by strong winds, resulting in the formations of \\u201ctafoni\\u201d cavities. 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fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/therma-hot-springs\\\/\\\">Therma Hot Springs<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/therma-hot-springs\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Hot springs emerging at the foot of the hill of Profitis Ilias in the Therma region have been used since ancient times. At a temperature of 42-44 degrees Celsius, the water wells up from 2 springs at a depth of around 1200 meters. The water is safe to drink and ideal for balneotherapy. The existence [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.905384\",\"lng\":\"25.122017\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/therma-hot-springs\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Hot springs emerging at the foot of the hill of Profitis Ilias in the Therma region have been used since ancient times. At a temperature of 42-44 degrees Celsius, the water wells up from 2 springs at a depth of around 1200 meters. The water is safe to drink and ideal for balneotherapy. The existence [&hellip;]<\\\/p>\\n\",\"post_content\":\"Hot springs emerging at the foot of the hill of Profitis Ilias in the Therma region have been used since ancient times. At a temperature of 42-44 degrees Celsius, the water wells up from 2 springs at a depth of around 1200 meters. The water is safe to drink and ideal for balneotherapy.\\r\\n\\r\\nThe existence of hot springs is related to the existence of geological faults and active tectonic activity today. Surface waters find a way down into the crust through the discontinuities in the rocks. There, the water meets the magmatic chambers of Lemnos\\u2019 volcanoes, which were once active 20 million years ago and are now enriched with various minerals and gases. Water returns to the surface through the faults with the help of gases and gushes up in the form of hot springs.\\r\\n\\r\\nTherma\\u2019s original thermal bath infrastructure remains intact, including a tiny changing room and a stone bathtub built in the 16th century. The depiction of a route on a 1588 map that connects the Castle of Myrina with Therma and the hill of Profitis Ilias shows the importance of the location and its relationship with the island\\u2019s administrative center.\",\"post_title\":\"Therma Hot Springs\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/therma-hot-springs\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Therma Hot Springs\\\" width=\\\"300\\\" height=\\\"189\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/therma-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.905384\",\"%wpcf-longtitude%\":\"25.122017\",\"%wpcf-location%\":\"\\u0398\\u03ad\\u03c1\\u03bc\\u03b1\",\"%_wpgmp_metabox_latitude%\":\"39.905384\",\"%_wpgmp_metabox_longitude%\":\"25.122017\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"4\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/volcanos.png\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_wpml_location_migration_done%\":\"1\",\"%_wpml_word_count%\":\"{\\\"total\\\":211,\\\"to_translate\\\":{\\\"en\\\":211}}\",\"%_thumbnail_id%\":\"2982\",\"%_edit_lock%\":\"1655205684:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%b8%ce%b5%cf%81%ce%bc%ce%ae-%cf%80%ce%b7%ce%b3%ce%ae-%ce%b8%ce%ad%cf%81%ce%bc%ce%b1\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/18-\\u0398\\u03ad\\u03c1\\u03bc\\u03b1.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"19679\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/18-\\u0398\\u03ad\\u03c1\\u03bc\\u03b1-scaled.jpg, 18-\\u0398\\u03ad\\u03c1\\u03bc\\u03b1, \",\"%_et_pb_truncate_post%\":\"<p>Hot springs emerging at the foot of the hill of Profitis Ilias in the Therma region have been used since ancient times. At a temperature of 42-44 degrees Celsius, the water wells up from 2 springs at a depth of around 1200 meters. The water is safe to drink and ideal for balneotherapy.<\\\/p>\\n<p>The existence of hot springs is related to the existence of geological faults and active tectonic activity today. Surface waters find a way down into the crust through the discontinuities in the rocks. There, the water meets the magmatic chambers of Lemnos\\u2019 volcanoes, which were once active 20 million years ago and are now enriched with various minerals and gases. Water returns to the surface through the faults with the help of gases and gushes up in the form of hot springs.<\\\/p>\\n<p>Therma\\u2019s original thermal bath infrastructure remains intact, including a tiny changing room and a stone bathtub built in the 16th century. 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class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kodias-volcanic-dome\\\/\\\">Kodias Volcanic Dome<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kodias-volcanic-dome\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Alongside the Myrina-Kodias road, the Kodias Volcanic Dome stands out in strong contrast to the flat surrounding landscape. The hill consists of dacitic lava which was formed 19.3-18.2 million years ago. The Kodias Volcanic Dome is a part of the wider group of volcanic structures that characterize the south-west region of Lemnos. Rising magma, rich [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.863\",\"lng\":\"25.147\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kodias-volcanic-dome\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Alongside the Myrina-Kodias road, the Kodias Volcanic Dome stands out in strong contrast to the flat surrounding landscape. The hill consists of dacitic lava which was formed 19.3-18.2 million years ago. The Kodias Volcanic Dome is a part of the wider group of volcanic structures that characterize the south-west region of Lemnos. Rising magma, rich [&hellip;]<\\\/p>\\n\",\"post_content\":\"Alongside the Myrina-Kodias road, the Kodias Volcanic Dome stands out in strong contrast to the flat surrounding landscape.\\r\\n\\r\\nThe hill consists of dacitic lava which was formed 19.3-18.2 million years ago. The Kodias Volcanic Dome is a part of the wider group of volcanic structures that characterize the south-west region of Lemnos.\\r\\n\\r\\nRising magma, rich in gas content, moved up most likely through tectonic faults and created this structure. 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The Kodias Volcanic Dome is a part of the wider group of volcanic structures that characterize the south-west region of Lemnos.<\\\/p>\\n<p>Rising magma, rich in gas content, moved up most likely through tectonic faults and created this structure. 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class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/evgatis-volcanic-dome\\\/\\\">Evgatis Volcanic Dome<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/evgatis-volcanic-dome\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The Evgatis Volcanic Dome is located in the southwest region of Lemnos, east of the town of Thanos. Composed of trachyandesite, the volcanic hill\\u2019s shape is characterized by steep and rugged slopes which are associated with the intense volcanic activity that caused magma to rise 19.3-18.2 million years ago. The activity that created this volcanic [&hellip;]<\\\/p>\\n\",\"address\":\"V436+XF \\u039c\\u03cd\\u03c1\\u03b9\\u03bd\\u03b1, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.854884693219134\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.111171298980718\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/evgatis-volcanic-dome\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The Evgatis Volcanic Dome is located in the southwest region of Lemnos, east of the town of Thanos. Composed of trachyandesite, the volcanic hill\\u2019s shape is characterized by steep and rugged slopes which are associated with the intense volcanic activity that caused magma to rise 19.3-18.2 million years ago. The activity that created this volcanic [&hellip;]<\\\/p>\\n\",\"post_content\":\"The Evgatis Volcanic Dome is located in the southwest region of Lemnos, east of the town of Thanos. Composed of trachyandesite, the volcanic hill\\u2019s shape is characterized by steep and rugged slopes which are associated with the intense volcanic activity that caused magma to rise 19.3-18.2 million years ago. The activity that created this volcanic dome is responsible for the formation of a series of other volcanic domes that are scattered throughout western Lemnos.\\r\\n\\r\\nDuring this period of time, viscous magma with a high content of potassium and silicon permeated into the geological formation through faults in the earth\\u2019s crust. 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Composed of trachyandesite, the volcanic hill\\u2019s shape is characterized by steep and rugged slopes which are associated with the intense volcanic activity that caused magma to rise 19.3-18.2 million years ago. The activity that created this volcanic dome is responsible for the formation of a series of other volcanic domes that are scattered throughout western Lemnos.<\\\/p>\\n<p>During this period of time, viscous magma with a high content of potassium and silicon permeated into the geological formation through faults in the earth\\u2019s crust. This resulted in the general uplifting of the area. 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class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/myrina-volcanic-dome\\\/\\\">Myrina Volcanic Dome<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/myrina-volcanic-dome\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The impressive peninsula, upon which the byzantine castle of Myrina is built, lies between two sandy beaches, Roman and the Turkish Gialos. This peninsula was formed 19.3-18.2 million years ago, when the intense volcanic activity caused dacitic magma to rise and permeate the crust, where it cooled instantly, creating the steep volcanic dome that characterizes [&hellip;]<\\\/p>\\n\",\"address\":\"V3G3+RG \\u039c\\u03cd\\u03c1\\u03b9\\u03bd\\u03b1, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.877058416910906\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.053927116394032\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/myrina-volcanic-dome\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The impressive peninsula, upon which the byzantine castle of Myrina is built, lies between two sandy beaches, Roman and the Turkish Gialos. This peninsula was formed 19.3-18.2 million years ago, when the intense volcanic activity caused dacitic magma to rise and permeate the crust, where it cooled instantly, creating the steep volcanic dome that characterizes [&hellip;]<\\\/p>\\n\",\"post_content\":\"The impressive peninsula, upon which the byzantine castle of Myrina is built, lies between two sandy beaches, Roman and the Turkish Gialos. This peninsula was formed 19.3-18.2 million years ago, when the intense volcanic activity caused dacitic magma to rise and permeate the crust, where it cooled instantly, creating the steep volcanic dome that characterizes the area.\\r\\n\\r\\nThe volcanic rock is porphyritic, meaning mineral crystals can be distinguished easily in the glassy mass. 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The fault is visible as a morphological rise in the hills east of the village. It is a large tectonic surface with a length of 11 km and a direction of NW-SE that was caused by recent seismic activity in the area that led the [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.935\",\"lng\":\"25.068\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kaspakas-fault\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The Kaspakas active fault appears north of the Kaspakas village. The fault is visible as a morphological rise in the hills east of the village. It is a large tectonic surface with a length of 11 km and a direction of NW-SE that was caused by recent seismic activity in the area that led the [&hellip;]<\\\/p>\\n\",\"post_content\":\"The Kaspakas active fault appears north of the Kaspakas village. The fault is visible as a morphological rise in the hills east of the village. It is a large tectonic surface with a length of 11 km and a direction of NW-SE that was caused by recent seismic activity in the area that led the rock to break.\\r\\n\\r\\nFaults are geological structures formed when strain in the Earth\\u2019s crust exceed the limit of rock strength, forcing it to break. The evidence of rock movement appears on the surface of the fault as scratches which are referred to as slip lines. These lines are critical for understanding the fault\\u2019s seismic activity.\\r\\n\\r\\nThe Kaspakas fault links rock formations of different ages together, specifically volcanic rocks (Upper Oligocene \\u2013 Middle Miocene) and Molassic sediments (Eocene).\",\"post_title\":\"Kaspakas Fault\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kaspakas-fault\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Kaspakas Fault\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/2-\\u03a1\\u03ae\\u03b3\\u03bc\\u03b1-\\u039a\\u03ac\\u03c3\\u03c0\\u03b1\\u03ba\\u03b1-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.935\",\"%wpcf-longtitude%\":\"25.068\",\"%wpcf-location%\":\"\\u039a\\u03ac\\u03c3\\u03c0\\u03b1\\u03ba\\u03b1\",\"%_wpgmp_metabox_latitude%\":\"39.935\",\"%_wpgmp_metabox_longitude%\":\"25.068\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"5\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/tectonic.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%wpcf-code%\":\"\",\"%_wpml_location_migration_done%\":\"1\",\"%_wpml_word_count%\":\"{\\\"total\\\":149,\\\"to_translate\\\":{\\\"en\\\":149}}\",\"%_thumbnail_id%\":\"2753\",\"%_edit_lock%\":\"1655206720:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%81%ce%ae%ce%b3%ce%bc%ce%b1-%ce%ba%ce%ac%cf%83%cf%80%ce%b1%ce%ba%ce%b1\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/2-\\u03a1\\u03ae\\u03b3\\u03bc\\u03b1-\\u039a\\u03ac\\u03c3\\u03c0\\u03b1\\u03ba\\u03b1.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"19834, 19835\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/2-\\u03ba\\u03ac\\u03c3\\u03c0\\u03b1\\u03ba\\u03b1\\u03c2-scaled.jpg, 2-\\u03ba\\u03ac\\u03c3\\u03c0\\u03b1\\u03ba\\u03b1\\u03c2, \",\"%_et_pb_truncate_post%\":\"<p>The Kaspakas active fault appears north of the Kaspakas village. The fault is visible as a morphological rise in the hills east of the village. It is a large tectonic surface with a length of 11 km and a direction of NW-SE that was caused by recent seismic activity in the area that led the rock to break.<\\\/p>\\n<p>Faults are geological structures formed when strain in the Earth\\u2019s crust exceed the limit of rock strength, forcing it to break. The evidence of rock movement appears on the surface of the fault as scratches which are referred to as slip lines. 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geosites\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/tectonic_result-small.png\"},\"id\":3569,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/tectonic_result-small.png\",\"name\":\"\\u03a4\\u03b5\\u03ba\\u03c4\\u03bf\\u03bd\\u03b9\\u03ba\\u03bf\\u03af\",\"id\":\"5\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"St. Charalambos Plakas Fault\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"St. Charalambos Plakas Fault\\\" width=\\\"300\\\" height=\\\"221\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/35-\\u0386\\u03b3\\u03b9\\u03bf\\u03c2-\\u03a7\\u03b1\\u03c1\\u03ac\\u03bb\\u03b1\\u03bc\\u03c0\\u03bf\\u03c2-\\u03a0\\u03bb\\u03ac\\u03ba\\u03b1\\u03c2-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding 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A large fault cuts through the area\\u2019s geological layers of sedimentary rocks. It is a normal fault with a NW-SE direction. The fault runs along the beach, right next to [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"40.0198\",\"lng\":\"25.4164\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/st-charalambos-plakas-fault\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Alterations of sandstone and clay geological formations, typical of Lemnos\\u2019s molassic deposits, are found northwest of the Plaka settlement, in the area of Saint Charalambos. A large fault cuts through the area\\u2019s geological layers of sedimentary rocks. It is a normal fault with a NW-SE direction. The fault runs along the beach, right next to [&hellip;]<\\\/p>\\n\",\"post_content\":\"Alterations of sandstone and clay geological formations, typical of Lemnos\\u2019s molassic deposits, are found northwest of the Plaka settlement, in the area of Saint Charalambos. A large fault cuts through the area\\u2019s geological layers of sedimentary rocks.\\r\\n\\r\\nIt is a normal fault with a NW-SE direction. The fault runs along the beach, right next to the steps leading down to the church\\u2019s holy water, where the movement of the geological formations on the vertical slope may be seen.\\r\\n\\r\\nThe evidence of rock movement is visible on the surface of the fault as fractures known as striations. These tectonic lines were formed by the friction of the rocks in their parallel movement and provide crucial information about the fault\\u2019s seismic activity in the past.\",\"post_title\":\"St. Charalambos Plakas Fault\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/st-charalambos-plakas-fault\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"St. Charalambos Plakas Fault\\\" width=\\\"300\\\" height=\\\"221\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/35-\\u0386\\u03b3\\u03b9\\u03bf\\u03c2-\\u03a7\\u03b1\\u03c1\\u03ac\\u03bb\\u03b1\\u03bc\\u03c0\\u03bf\\u03c2-\\u03a0\\u03bb\\u03ac\\u03ba\\u03b1\\u03c2-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" 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Clays and sandstones with interstitial cobblestones (rock with rounded pebbles within) in the lower layers, aged about 23 [&hellip;]<\\\/p>\\n\",\"address\":\"V83X+XH \\u039c\\u03bf\\u03cd\\u03b4\\u03c1\\u03bf\\u03c2, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.854896914322005\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.34899999734496\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/poliochni-harbour-fault\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The stratigraphic contact of two separate geological formations, particularly the upper molassic sediments of Lemnos and the pyroclastic formations of Romanos, is located north of the ancient site of Poliochni on the slopes of the scenic harbor. Clays and sandstones with interstitial cobblestones (rock with rounded pebbles within) in the lower layers, aged about 23 [&hellip;]<\\\/p>\\n\",\"post_content\":\"The stratigraphic contact of two separate geological formations, particularly the upper molassic sediments of Lemnos and the pyroclastic formations of Romanos, is located north of the ancient site of Poliochni on the slopes of the scenic harbor. Clays and sandstones with interstitial cobblestones (rock with rounded pebbles within) in the lower layers, aged about 23 million years, can be found with a general dip direction to the NW under the Lower Miocene tuff.\\r\\n\\r\\nMarine sedimentogenesis occurred between 22 and 28 million years ago, resulting in the sedimentary formations of Lemnos. Around 22 million years ago, the earliest volcanic products of Lemnos, pyroclastic rocks with layers of volcanic ash with various rock fragments, settled over these sedimentary rocks.\\r\\n\\r\\nAt this location, the movement of tectonic faults in the NE-SW direction alters the layers and brings older sedimentary formations into contact with younger volcanic formations, resulting in a complicated geological picture.\",\"post_title\":\"Poliochni (harbour) Fault\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/poliochni-harbour-fault\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Poliochni (harbour) Fault\\\" width=\\\"300\\\" height=\\\"209\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/46-\\u03a0\\u03bf\\u03bb\\u03b9\\u03cc\\u03c7\\u03bd\\u03b7-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.85489\",\"%wpcf-longtitude%\":\"25.34899\",\"%wpcf-location%\":\"\\u039b\\u03b9\\u03bc\\u03ac\\u03bd\\u03b9 \\u0392\\u03bf\\u03c1\\u03bf\\u03c3\\u03ba\\u03cc\\u03c0\\u03bf\\u03c5\",\"%_wpgmp_metabox_latitude%\":\"39.854896914322005\",\"%_wpgmp_metabox_longitude%\":\"25.34899999734496\",\"%_wpgmp_location_address%\":\"V83X+XH \\u039c\\u03bf\\u03cd\\u03b4\\u03c1\\u03bf\\u03c2, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"%_wpgmp_location_city%\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"5\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/tectonic.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%wpcf-code%\":\"\",\"%_wpml_location_migration_done%\":\"1\",\"%_wpml_word_count%\":\"{\\\"total\\\":155,\\\"to_translate\\\":{\\\"en\\\":155}}\",\"%_thumbnail_id%\":\"2738\",\"%_edit_lock%\":\"1655207084:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%81%ce%ae%ce%b3%ce%bc%ce%b1-%cf%80%ce%bf%ce%bb%ce%b9%cf%8c%cf%87%ce%bd%ce%b7%cf%82-%ce%bb%ce%b9%ce%bc%ce%ac%ce%bd%ce%b9\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/46-\\u03a0\\u03bf\\u03bb\\u03b9\\u03cc\\u03c7\\u03bd\\u03b7.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"19911\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/46-\\u03a0\\u03bf\\u03bb\\u03b9\\u03cc\\u03c7\\u03bd\\u03b7.jpg, 46-\\u03a0\\u03bf\\u03bb\\u03b9\\u03cc\\u03c7\\u03bd\\u03b7, \",\"%_et_pb_truncate_post%\":\"<p>The stratigraphic contact of two separate geological formations, particularly the upper molassic sediments of Lemnos and the pyroclastic formations of Romanos, is located north of the ancient site of Poliochni on the slopes of the scenic harbor. Clays and sandstones with interstitial cobblestones (rock with rounded pebbles within) in the lower layers, aged about 23 million years, can be found with a general dip direction to the NW under the Lower Miocene tuff.<\\\/p>\\n<p>Marine sedimentogenesis occurred between 22 and 28 million years ago, resulting in the sedimentary formations of Lemnos. 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class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-kavalaris-fault\\\/\\\">Cape Kavalaris Fault<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-kavalaris-fault\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The extension of Roussopouli fault leads to the formation of Kavalaris Cape on the east coast of Lemnos. The tectonic structure may be seen east of the church of Agia Kyriaki, where parallel ruptured surfaces define the volcanic rocks and construct the shoreline to Keros Bay. The Roussopouli Fault runs for roughly 10 km in [&hellip;]<\\\/p>\\n\",\"address\":\"Unnamed Road, \\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2 814 01, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.88921424833805\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.361424294998173\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-kavalaris-fault\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The extension of Roussopouli fault leads to the formation of Kavalaris Cape on the east coast of Lemnos. The tectonic structure may be seen east of the church of Agia Kyriaki, where parallel ruptured surfaces define the volcanic rocks and construct the shoreline to Keros Bay. The Roussopouli Fault runs for roughly 10 km in [&hellip;]<\\\/p>\\n\",\"post_content\":\"The extension of Roussopouli fault leads to the formation of Kavalaris Cape on the east coast of Lemnos.\\r\\nThe tectonic structure may be seen east of the church of Agia Kyriaki, where parallel ruptured surfaces define the volcanic rocks and construct the shoreline to Keros Bay.\\r\\n\\r\\nThe Roussopouli Fault runs for roughly 10 km in a NE-SW direction and separates the Lower Miocene pyroclastic rocks from the Oligocene sedimentary formations overlaid by recent alluvial and coastal deposits.\",\"post_title\":\"Cape Kavalaris Fault\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-kavalaris-fault\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Cape Kavalaris Fault\\\" width=\\\"300\\\" height=\\\"210\\\" 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geosites\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/tectonic_result-small.png\"},\"id\":3573,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/tectonic_result-small.png\",\"name\":\"\\u03a4\\u03b5\\u03ba\\u03c4\\u03bf\\u03bd\\u03b9\\u03ba\\u03bf\\u03af\",\"id\":\"5\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Cape Ropalo Coastal Tectonic Formations\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Cape Ropalo Coastal Tectonic Formations\\\" width=\\\"300\\\" height=\\\"210\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/9-\\u0391\\u03ba\\u03c1\\u03c9\\u03c4\\u03ae\\u03c1\\u03b9\\u03bf-\\u03a1\\u03cc\\u03c0\\u03b1\\u03bb\\u03bf-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-ropalo-coastal-tectonic-formations\\\/\\\">Cape Ropalo Coastal Tectonic Formations<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-ropalo-coastal-tectonic-formations\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The southwest end of Lemnos is defined by two capes, Tigani to the west and Ropalo to the east. The presence of geological faults that split the volcanic rocks and form the tectonic coastline terrain, determines the area\\u2019s geomorphology. The eastern edge of Cape Ropalo, in particular, is produced by a sequence of faults oriented [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.832974\",\"lng\":\"25.053158\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-ropalo-coastal-tectonic-formations\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The southwest end of Lemnos is defined by two capes, Tigani to the west and Ropalo to the east. The presence of geological faults that split the volcanic rocks and form the tectonic coastline terrain, determines the area\\u2019s geomorphology. The eastern edge of Cape Ropalo, in particular, is produced by a sequence of faults oriented [&hellip;]<\\\/p>\\n\",\"post_content\":\"The southwest end of Lemnos is defined by two capes, Tigani to the west and Ropalo to the east. The presence of geological faults that split the volcanic rocks and form the tectonic coastline terrain, determines the area\\u2019s geomorphology.\\r\\n\\r\\nThe eastern edge of Cape Ropalo, in particular, is produced by a sequence of faults oriented NNW-SSE, which impact the 18.2-19.3 million year old volcanic formations that define Cape Ropalo.\",\"post_title\":\"Cape Ropalo Coastal Tectonic Formations\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-ropalo-coastal-tectonic-formations\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Cape Ropalo Coastal Tectonic Formations\\\" width=\\\"300\\\" height=\\\"210\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/9-\\u0391\\u03ba\\u03c1\\u03c9\\u03c4\\u03ae\\u03c1\\u03b9\\u03bf-\\u03a1\\u03cc\\u03c0\\u03b1\\u03bb\\u03bf-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.832974\",\"%wpcf-longtitude%\":\"25.053158\",\"%wpcf-location%\":\"\\u0391\\u03ba\\u03c1\\u03c9\\u03c4\\u03ae\\u03c1\\u03b9 \\u03a1\\u03cc\\u03c0\\u03b1\\u03bb\\u03bf\",\"%_wpgmp_metabox_latitude%\":\"39.832974\",\"%_wpgmp_metabox_longitude%\":\"25.053158\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"5\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/tectonic.png\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_wpml_location_migration_done%\":\"1\",\"%_wpml_word_count%\":\"{\\\"total\\\":81,\\\"to_translate\\\":{\\\"en\\\":81}}\",\"%_thumbnail_id%\":\"2756\",\"%_edit_lock%\":\"1655207391:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%81%ce%b7%ce%be%ce%b9%ce%b3%ce%b5%ce%bd%ce%ae%cf%82-%ce%b1%ce%ba%cf%84%ce%ae-%ce%b1%ce%ba%cf%81%cf%89%cf%84%ce%ae%cf%81%ce%b9%ce%bf-%cf%81%cf%8c%cf%80%ce%b1%ce%bb%ce%bf\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/9-\\u0391\\u03ba\\u03c1\\u03c9\\u03c4\\u03ae\\u03c1\\u03b9\\u03bf-\\u03a1\\u03cc\\u03c0\\u03b1\\u03bb\\u03bf.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"19983\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/9-\\u0391\\u03ba\\u03c1\\u03c9\\u03c4\\u03ae\\u03c1\\u03b9\\u03bf-\\u03a1\\u03cc\\u03c0\\u03b1\\u03bb\\u03bf.jpg, 9-\\u0391\\u03ba\\u03c1\\u03c9\\u03c4\\u03ae\\u03c1\\u03b9\\u03bf \\u03a1\\u03cc\\u03c0\\u03b1\\u03bb\\u03bf, \",\"%_et_pb_truncate_post%\":\"<p>The southwest end of Lemnos is defined by two capes, Tigani to the west and Ropalo to the east. 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An impressive geological structure in the coastal zone impacts the area\\u2019s molassic formations. A system of normal faults cuts the geological formations almost entirely along the [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.80671\",\"lng\":\"25.362923\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-st-sozon-fault-formations\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Huge alternations between geological formations of sandstone and clay layers, typical of Lemnos\\u2019 molassic deposits, appear near the church of Agios Sozontas in the southeastern end of the island. An impressive geological structure in the coastal zone impacts the area\\u2019s molassic formations. A system of normal faults cuts the geological formations almost entirely along the [&hellip;]<\\\/p>\\n\",\"post_content\":\"Huge alternations between geological formations of sandstone and clay layers, typical of Lemnos\\u2019 molassic deposits, appear near the church of Agios Sozontas in the southeastern end of the island.\\r\\n\\r\\nAn impressive geological structure in the coastal zone impacts the area\\u2019s molassic formations. A system of normal faults cuts the geological formations almost entirely along the length of the beach, causing significant deformation and movement of the geological layers along the faulting planes.\",\"post_title\":\"Cape St. Sozon Fault Formations\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-st-sozon-fault-formations\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Cape St. Sozon Fault Formations\\\" width=\\\"300\\\" height=\\\"209\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/48-\\u0386\\u03b3\\u03b9\\u03bf\\u03c2-\\u03a3\\u03ce\\u03b6\\u03c9\\u03bd-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" 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The existence of faults system in sedimentary rocks dating back 34-37 million years (Eocene \\u2013 Oligocene) and, more particularly, the alternations of sandstones and clays in which layers of tuffites appear, characterize the region. Opposite the church [&hellip;]<\\\/p>\\n\",\"post_content\":\"The peninsula of St. Sotira is located at the northeastern end of Lemnos, west of the Plaka peninsula. The existence of faults system in sedimentary rocks dating back 34-37 million years (Eocene \\u2013 Oligocene) and, more particularly, the alternations of sandstones and clays in which layers of tuffites appear, characterize the region.\\r\\n\\r\\nOpposite the church of Agia Sotira along the coastal slope, the layers exhibit an impressive curve which are interrupted by repeated regular fractures that form a distinctive image.\\r\\n\\r\\nNorth of the church of Agia Sotira, at the end of the road, is the scenic harbor which is part of the ruins of the old port. 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geosites\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/tectonic_result-small.png\"},\"id\":3578,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/tectonic_result-small.png\",\"name\":\"\\u03a4\\u03b5\\u03ba\\u03c4\\u03bf\\u03bd\\u03b9\\u03ba\\u03bf\\u03af\",\"id\":\"5\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Roussopouli Fault\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Roussopouli Fault\\\" width=\\\"300\\\" height=\\\"193\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/43-\\u03c1\\u03b7\\u03b3\\u03bc\\u03b1-\\u03c1\\u03bf\\u03c5\\u03c3\\u03c3\\u03bf\\u03c0\\u03bf\\u03c5\\u03bb\\u03b9-scaled-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/roussopouli-fault\\\/\\\">Roussopouli Fault<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/roussopouli-fault\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The Roussopouli fault is a large tectonic structure about 10 km long that runs ENE-WSW and connects two different geological formations. The pyroclastic rocks are around 23 million years old (Lower Miocene), while the sedimentary rocks are approximately 33 million years old (Upper Eocene \\u2013 Lower Oligocene). The tectonic structure generates an extended terrace on [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.879009\",\"lng\":\"25.30808\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/roussopouli-fault\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The Roussopouli fault is a large tectonic structure about 10 km long that runs ENE-WSW and connects two different geological formations. The pyroclastic rocks are around 23 million years old (Lower Miocene), while the sedimentary rocks are approximately 33 million years old (Upper Eocene \\u2013 Lower Oligocene). The tectonic structure generates an extended terrace on [&hellip;]<\\\/p>\\n\",\"post_content\":\"The Roussopouli fault is a large tectonic structure about 10 km long that runs ENE-WSW and connects two different geological formations. The pyroclastic rocks are around 23 million years old (Lower Miocene), while the sedimentary rocks are approximately 33 million years old (Upper Eocene \\u2013 Lower Oligocene).\\r\\n\\r\\nThe tectonic structure generates an extended terrace on the area\\u2019s gentle landscape. It begins at Cape Sagrada, south of the village of Moudros, continues near to the settlement of Roussopouli, and terminates at Cape Kavalaris, in the harbor of Keros.\",\"post_title\":\"Roussopouli Fault\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/roussopouli-fault\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Roussopouli Fault\\\" width=\\\"300\\\" height=\\\"193\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/43-\\u03c1\\u03b7\\u03b3\\u03bc\\u03b1-\\u03c1\\u03bf\\u03c5\\u03c3\\u03c3\\u03bf\\u03c0\\u03bf\\u03c5\\u03bb\\u03b9-scaled-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.879009\",\"%wpcf-longtitude%\":\"25.30808\",\"%_wpgmp_metabox_latitude%\":\"39.879009\",\"%_wpgmp_metabox_longitude%\":\"25.30808\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"5\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/tectonic.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%wpcf-location%\":\"\",\"%wpcf-code%\":\"\",\"%_wpml_location_migration_done%\":\"1\",\"%_wpml_word_count%\":\"{\\\"total\\\":96,\\\"to_translate\\\":{\\\"en\\\":96}}\",\"%_thumbnail_id%\":\"2998\",\"%_edit_lock%\":\"1655209909:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%81%ce%ae%ce%b3%ce%bc%ce%b1-%cf%81%ce%bf%cf%85%cf%83%cf%83%ce%bf%cf%80%ce%bf%cf%85%ce%bb%ce%af%ce%bf%cf%85\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/43-\\u03c1\\u03b7\\u03b3\\u03bc\\u03b1-\\u03c1\\u03bf\\u03c5\\u03c3\\u03c3\\u03bf\\u03c0\\u03bf\\u03c5\\u03bb\\u03b9.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20097\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/43-\\u03c1\\u03b7\\u03b3\\u03bc\\u03b1-\\u03c1\\u03bf\\u03c5\\u03c3\\u03c3\\u03bf\\u03c0\\u03bf\\u03c5\\u03bb\\u03b9-scaled.jpg, 43-\\u03c1\\u03b7\\u03b3\\u03bc\\u03b1 \\u03c1\\u03bf\\u03c5\\u03c3\\u03c3\\u03bf\\u03c0\\u03bf\\u03c5\\u03bb\\u03b9, \",\"%_et_pb_truncate_post%\":\"<p>The Roussopouli fault is a large tectonic structure about 10 km long that runs ENE-WSW and connects two different geological formations. The pyroclastic rocks are around 23 million years old (Lower Miocene), while the sedimentary rocks are approximately 33 million years old (Upper Eocene \\u2013 Lower Oligocene).<\\\/p>\\n<p>The tectonic structure generates an extended terrace on the area\\u2019s gentle landscape. 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fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/pachymnos-fault\\\/\\\">Pachymnos Fault<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/pachymnos-fault\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The Pachymnos fault located towards the southeastern end of Lemnos, a few kilometers from Thanos settlement. West of the road can be seen the fault surface that forms an impressive steep slope extending to the sea. Faults are geological structures formed when tensions inside the Earth\\u2019s crust overpass the limits of rock strength, forcing it [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.845290\",\"lng\":\"25.057745\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/pachymnos-fault\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The Pachymnos fault located towards the southeastern end of Lemnos, a few kilometers from Thanos settlement. West of the road can be seen the fault surface that forms an impressive steep slope extending to the sea. Faults are geological structures formed when tensions inside the Earth\\u2019s crust overpass the limits of rock strength, forcing it [&hellip;]<\\\/p>\\n\",\"post_content\":\"The Pachymnos fault located towards the southeastern end of Lemnos, a few kilometers from Thanos settlement. West of the road can be seen the fault surface that forms an impressive steep slope extending to the sea.\\r\\n\\r\\nFaults are geological structures formed when tensions inside the Earth\\u2019s crust overpass the limits of rock strength, forcing it to break.\\r\\n\\r\\nThe nearly vertical and smooth surface is the tectonic surface of the fault, created by recent seismic activity in the area which caused the volcanic rocks to break. On this surface, the traces of rock movement emerge as slip lines (scratches). 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fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-mourtzeflos\\\/\\\">Cape Mourtzeflos<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-mourtzeflos\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The Cape of Mourtzeflos marks the farthest northwest side of Lemnos. The volcanic formation called the volcanic dome of Mourtzeflos appears as an islet composed of volcanic rocks of tracheandesitic composition, but it is joined to the mainland by a small sandy strip, forming the tombolo\\u2019s unique geomorphological structure. Approximately 20-21 million years old, the [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.985\",\"lng\":\"25.041\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-mourtzeflos\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The Cape of Mourtzeflos marks the farthest northwest side of Lemnos. The volcanic formation called the volcanic dome of Mourtzeflos appears as an islet composed of volcanic rocks of tracheandesitic composition, but it is joined to the mainland by a small sandy strip, forming the tombolo\\u2019s unique geomorphological structure. Approximately 20-21 million years old, the [&hellip;]<\\\/p>\\n\",\"post_content\":\"The Cape of Mourtzeflos marks the farthest northwest side of Lemnos. The volcanic formation called the volcanic dome of Mourtzeflos appears as an islet composed of volcanic rocks of tracheandesitic composition, but it is joined to the mainland by a small sandy strip, forming the tombolo\\u2019s unique geomorphological structure.\\r\\n\\r\\nApproximately 20-21 million years old, the volcanic structure\\u2019s formation is linked to a series of volcanic structures that were created on Western Lemnos during that period. These distinctive volcanic domes were formed by ascending viscous magma with a high gas content that penetrated the pre-existing sedimentary rocks, folding and uplifting them. In many cases, the magma either reached the surface as thick lava or, after cooling at a shallow depth below the surface, was revealed by the erosion of the overlying geologic material, resulting in the formation of these distinctive volcanic structures in both cases.\\r\\n\\r\\nThe morphology of the coast and the separation of the islet from its adjoining land are the result of the movement of the NE-SW large Mourtzeflos strike-slip fault.\\r\\n\\r\\nTombolo is a coastal deposition formation composed primarily of sands and rounded pebbles (cobbles). The formation of a tombolo is formed by the impact of sea waves and the reduction of their transport capacity, resulting the deposition of sediments which are filling the seabed and its eventual emergence from the water surface.\",\"post_title\":\"Cape Mourtzeflos\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-mourtzeflos\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Cape Mourtzeflos\\\" width=\\\"300\\\" height=\\\"242\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/1-\\u039c\\u03bf\\u03c5\\u03c1\\u03c4\\u03b6\\u03bf\\u03c5\\u03c6\\u03bb\\u03bf\\u03c2-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.985\",\"%wpcf-longtitude%\":\"25.041\",\"%wpcf-location%\":\"\\u039c\\u03bf\\u03cd\\u03c1\\u03c4\\u03b6\\u03bf\\u03c5\\u03c6\\u03bb\\u03bf\",\"%_wpgmp_metabox_latitude%\":\"39.985\",\"%_wpgmp_metabox_longitude%\":\"25.041\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"14\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi.png\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_wpml_location_migration_done%\":\"1\",\"%_wpml_word_count%\":\"{\\\"total\\\":235,\\\"to_translate\\\":{\\\"en\\\":235}}\",\"%_thumbnail_id%\":\"2782\",\"%_edit_lock%\":\"1655213923:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%b1%ce%ba%cf%81%cf%89%cf%84%ce%ae%cf%81%ce%b9%ce%bf-%ce%bc%ce%bf%cf%8d%cf%81%cf%84%ce%b6%ce%b5%cf%86%ce%bb%ce%bf%cf%82\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/1-\\u039c\\u03bf\\u03c5\\u03c1\\u03c4\\u03b6\\u03bf\\u03c5\\u03c6\\u03bb\\u03bf\\u03c2.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20169\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/1-\\u039c\\u03bf\\u03c5\\u03c1\\u03c4\\u03b6\\u03bf\\u03c5\\u03c6\\u03bb\\u03bf\\u03c2.jpg, 1- \\u039c\\u03bf\\u03c5\\u03c1\\u03c4\\u03b6\\u03bf\\u03c5\\u03c6\\u03bb\\u03bf\\u03c2, \",\"%_et_pb_truncate_post%\":\"<p>The Cape of Mourtzeflos marks the farthest northwest side of Lemnos. The volcanic formation called the volcanic dome of Mourtzeflos appears as an islet composed of volcanic rocks of tracheandesitic composition, but it is joined to the mainland by a small sandy strip, forming the tombolo\\u2019s unique geomorphological structure.<\\\/p>\\n<p>Approximately 20-21 million years old, the volcanic structure\\u2019s formation is linked to a series of volcanic structures that were created on Western Lemnos during that period. These distinctive volcanic domes were formed by ascending viscous magma with a high gas content that penetrated the pre-existing sedimentary rocks, folding and uplifting them. In many cases, the magma either reached the surface as thick lava or, after cooling at a shallow depth below the surface, was revealed by the erosion of the overlying geologic material, resulting in the formation of these distinctive volcanic structures in both cases.<\\\/p>\\n<p>The morphology of the coast and the separation of the islet from its adjoining land are the result of the movement of the NE-SW large Mourtzeflos strike-slip fault.<\\\/p>\\n<p>Tombolo is a coastal deposition formation composed primarily of sands and rounded pebbles (cobbles). 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geosites\"},\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\"},\"id\":3582,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\",\"name\":\"\\u03a0\\u03b1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b9\\u03bf\\u03b9\",\"id\":\"14\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Filoktitis \\u2013 Kaveria Cave\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Filoktitis \\u2013 Kaveria Cave\\\" width=\\\"300\\\" height=\\\"155\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/32-\\u03a3\\u03c0\\u03b7\\u03bb\\u03b9\\u03ac-\\u03c4\\u03bf\\u03c5-\\u03a6\\u03b9\\u03bb\\u03bf\\u03ba\\u03c4\\u03ae\\u03c4\\u03b7-\\u039a\\u03b1\\u03b2\\u03b5\\u03af\\u03c1\\u03b9\\u03b13-scaled-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/filoktitis-kaveria-cave\\\/\\\">Filoktitis \\u2013 Kaveria Cave<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/filoktitis-kaveria-cave\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The cave of Filoktitis is located on the northeast coast of Lemnos near the archaeological complex of the Temple of Kaveria, one of Lemnos\\u2019 most important archaeological sites. A large concave has opened in the area\\u2019s sandstone cliffs going down towards the sea. Descending the steps carved into the sandstone rocks, the visitor reaches the [&hellip;]<\\\/p>\\n\",\"address\":\"X8JR+8R \\u039c\\u03bf\\u03cd\\u03b4\\u03c1\\u03bf\\u03c2, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.98077489984695\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.342096941406254\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/filoktitis-kaveria-cave\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The cave of Filoktitis is located on the northeast coast of Lemnos near the archaeological complex of the Temple of Kaveria, one of Lemnos\\u2019 most important archaeological sites. A large concave has opened in the area\\u2019s sandstone cliffs going down towards the sea. Descending the steps carved into the sandstone rocks, the visitor reaches the [&hellip;]<\\\/p>\\n\",\"post_content\":\"The cave of Filoktitis is located on the northeast coast of Lemnos near the archaeological complex of the Temple of Kaveria, one of Lemnos\\u2019 most important archaeological sites.\\r\\n\\r\\nA large concave has opened in the area\\u2019s sandstone cliffs going down towards the sea. Descending the steps carved into the sandstone rocks, the visitor reaches the opening. Inside this crevice is the underwater cave of Filoktitis, which can also be accessed by boat from the sea.\\r\\n\\r\\nThe cave is a type of coastal erosion in which sea waves erode rocks along geological discontinuities. The area\\u2019s sedimentary molassic rocks, in particular, cannot resist to the erosion processes, resulting in the creation of coastal caverns.\\r\\n\\r\\nAccording to mythology, Philoktitis lived in this cave for around 10 years after being bitten in the leg by a snake, which caused him to depart from the ship bound for Troy to fight in the Trojan War.\",\"post_title\":\"Filoktitis \\u2013 Kaveria Cave\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/filoktitis-kaveria-cave\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Filoktitis \\u2013 Kaveria Cave\\\" width=\\\"300\\\" height=\\\"155\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/32-\\u03a3\\u03c0\\u03b7\\u03bb\\u03b9\\u03ac-\\u03c4\\u03bf\\u03c5-\\u03a6\\u03b9\\u03bb\\u03bf\\u03ba\\u03c4\\u03ae\\u03c4\\u03b7-\\u039a\\u03b1\\u03b2\\u03b5\\u03af\\u03c1\\u03b9\\u03b13-scaled-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.980\",\"%wpcf-longtitude%\":\"25.341\",\"%_wpgmp_metabox_latitude%\":\"39.98077489984695\",\"%_wpgmp_metabox_longitude%\":\"25.342096941406254\",\"%_wpgmp_location_address%\":\"X8JR+8R \\u039c\\u03bf\\u03cd\\u03b4\\u03c1\\u03bf\\u03c2, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"%_wpgmp_location_city%\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"14\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi.png\",\"%wpcf-location%\":\"\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_wpml_location_migration_done%\":\"1\",\"%_wpml_word_count%\":\"{\\\"total\\\":171,\\\"to_translate\\\":{\\\"en\\\":171}}\",\"%_thumbnail_id%\":\"3037\",\"%_edit_lock%\":\"1655276461:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%83%cf%80%ce%b7%ce%bb%ce%b9%ce%ac-%cf%84%ce%bf%cf%85-%cf%86%ce%b9%ce%bb%ce%bf%ce%ba%cf%84%ce%ae%cf%84%ce%b7-%ce%ba%ce%b1%ce%b2%ce%b5%ce%af%cf%81%ce%b9%ce%b1\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/32-\\u03a3\\u03c0\\u03b7\\u03bb\\u03b9\\u03ac-\\u03c4\\u03bf\\u03c5-\\u03a6\\u03b9\\u03bb\\u03bf\\u03ba\\u03c4\\u03ae\\u03c4\\u03b7-\\u039a\\u03b1\\u03b2\\u03b5\\u03af\\u03c1\\u03b9\\u03b13.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20207, 20208, 20209\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/32-\\u03a3\\u03c0\\u03b7\\u03bb\\u03b9\\u03ac-\\u03c4\\u03bf\\u03c5-\\u03a6\\u03b9\\u03bb\\u03bf\\u03ba\\u03c4\\u03ae\\u03c4\\u03b7-\\u039a\\u03b1\\u03b2\\u03b5\\u03af\\u03c1\\u03b9\\u03b12-scaled.jpg, 32-\\u03a3\\u03c0\\u03b7\\u03bb\\u03b9\\u03ac \\u03c4\\u03bf\\u03c5 \\u03a6\\u03b9\\u03bb\\u03bf\\u03ba\\u03c4\\u03ae\\u03c4\\u03b7-\\u039a\\u03b1\\u03b2\\u03b5\\u03af\\u03c1\\u03b9\\u03b12, \",\"%_et_pb_truncate_post%\":\"<p>The cave of Filoktitis is located on the northeast coast of Lemnos near the archaeological complex of the Temple of Kaveria, one of Lemnos\\u2019 most important archaeological sites.<\\\/p>\\n<p>A large concave has opened in the area\\u2019s sandstone cliffs going down towards the sea. 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class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/fanarakis-sea-caves\\\/\\\">Fanaraki&#8217;s Sea Caves<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/fanarakis-sea-caves\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Southwest of Moudros, the Cape of Aspros Kavos features pyroclastic deposits with considerable hydrothermal alteration at the beaches of \\\"Mikro\\\" and \\\"Megalo Fanaraki\\\". Mineralogical, chemical, and structural changes occurred in the surrounding strata as a result of the impact of hot solutions of metal-rich water flowing in the pyroclastic materials. These alterations have resulted in [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.852\",\"lng\":\"25.237\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/fanarakis-sea-caves\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Southwest of Moudros, the Cape of Aspros Kavos features pyroclastic deposits with considerable hydrothermal alteration at the beaches of \\\"Mikro\\\" and \\\"Megalo Fanaraki\\\". Mineralogical, chemical, and structural changes occurred in the surrounding strata as a result of the impact of hot solutions of metal-rich water flowing in the pyroclastic materials. 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geosites\"},\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\"},\"id\":3584,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\",\"name\":\"\\u03a0\\u03b1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b9\\u03bf\\u03b9\",\"id\":\"14\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Prassa Limani Tombolo\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Prassa Limani Tombolo\\\" width=\\\"300\\\" height=\\\"210\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/4-\\u03a4\\u03cc\\u03bc\\u03c0\\u03bf\\u03bb\\u03bf-\\u03a0\\u03c1\\u03b1\\u03c3\\u03c3\\u03ac-\\u039b\\u03b9\\u03bc\\u03ac\\u03bd\\u03b9-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/prassa-limani-tombolo\\\/\\\">Prassa Limani Tombolo<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/prassa-limani-tombolo\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The \\\"Prasa Limani\\\" Tombolo, found on the northern side of the Agios Ioannis beach, is the sandy path that links the volcanic rock to the shore. Rising magma penetrated and solidified in\\u00a0pre-existing volcanic rocks and\\u00a0formed\\u00a0the islet. Over time, erosion removed the surrounding rocks, exposing the volcanic vein. The tombolo is a coastal deposition formation composed [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.927\",\"lng\":\"25.067\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/prassa-limani-tombolo\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The \\\"Prasa Limani\\\" Tombolo, found on the northern side of the Agios Ioannis beach, is the sandy path that links the volcanic rock to the shore. Rising magma penetrated and solidified in\\u00a0pre-existing volcanic rocks and\\u00a0formed\\u00a0the islet. Over time, erosion removed the surrounding rocks, exposing the volcanic vein. 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The formation of a tombolo is formed by the impact of sea waves and the restriction of their transport capacity, which results in materials such as sand and pebbles collecting there, eventually producing a strip of land that connects the island to the nearby shore.\\r\\n\\r\\n<\\\/div>\",\"post_title\":\"Prassa Limani Tombolo\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/prassa-limani-tombolo\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Prassa Limani Tombolo\\\" width=\\\"300\\\" height=\\\"210\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/4-\\u03a4\\u03cc\\u03bc\\u03c0\\u03bf\\u03bb\\u03bf-\\u03a0\\u03c1\\u03b1\\u03c3\\u03c3\\u03ac-\\u039b\\u03b9\\u03bc\\u03ac\\u03bd\\u03b9-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.927\",\"%wpcf-longtitude%\":\"25.067\",\"%wpcf-location%\":\"\\u0386\\u03b3\\u03b9\\u03bf\\u03c2 \\u0399\\u03c9\\u03ac\\u03bd\\u03bd\\u03b7\\u03c2\",\"%_wpgmp_metabox_latitude%\":\"39.927\",\"%_wpgmp_metabox_longitude%\":\"25.067\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"14\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi.png\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2751\",\"%_edit_lock%\":\"1655279427:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%84%cf%8c%ce%bc%cf%80%ce%bf%ce%bb%ce%bf-%ce%b1%ce%b3%ce%af%ce%bf%cf%85-%ce%b9%cf%89%ce%ac%ce%bd%ce%bd%ce%b7\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/4-\\u03a4\\u03cc\\u03bc\\u03c0\\u03bf\\u03bb\\u03bf-\\u03a0\\u03c1\\u03b1\\u03c3\\u03c3\\u03ac-\\u039b\\u03b9\\u03bc\\u03ac\\u03bd\\u03b9.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20282\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/4-\\u03a4\\u03cc\\u03bc\\u03c0\\u03bf\\u03bb\\u03bf-\\u03a0\\u03c1\\u03b1\\u03c3\\u03c3\\u03ac-\\u039b\\u03b9\\u03bc\\u03ac\\u03bd\\u03b9.jpg, 4-\\u03a4\\u03cc\\u03bc\\u03c0\\u03bf\\u03bb\\u03bf \\u03a0\\u03c1\\u03b1\\u03c3\\u03c3\\u03ac \\u039b\\u03b9\\u03bc\\u03ac\\u03bd\\u03b9, \",\"%_et_pb_truncate_post%\":\"<p>The &#8220;Prasa Limani&#8221; Tombolo, found on the northern side of the Agios Ioannis beach, is the sandy path that links the volcanic rock to the shore.<\\\/p>\\n<p>Rising magma penetrated and solidified in\\u00a0pre-existing volcanic rocks and\\u00a0formed\\u00a0the islet. 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geosites\"},\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\"},\"id\":3586,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\",\"name\":\"\\u03a0\\u03b1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b9\\u03bf\\u03b9\",\"id\":\"14\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"St. Efthimia Tombolo\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"St. Efthimia Tombolo\\\" width=\\\"300\\\" height=\\\"210\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/13-\\u03a4\\u03cc\\u03bc\\u03c0\\u03bf\\u03bb\\u03bf-\\u0391\\u03b3\\u03af\\u03b1\\u03c2-\\u0395\\u03c5\\u03b8\\u03c5\\u03bc\\u03af\\u03b1\\u03c2-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/st-efthimia-tombolo\\\/\\\">St. Efthimia Tombolo<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/st-efthimia-tombolo\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The tombolo of St. Efthimia is located south of Lemnos, on the southwest shore of Cape \\\"Fakos\\\". The tombolo is a natural corridor composed of loose sediments that links the coast to the neighboring rocky islet. After being cut off from the nearby shore, the islet operated as a seawall, causing the sea waves to [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.809040\",\"lng\":\"25.141208\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/st-efthimia-tombolo\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The tombolo of St. Efthimia is located south of Lemnos, on the southwest shore of Cape \\\"Fakos\\\". The tombolo is a natural corridor composed of loose sediments that links the coast to the neighboring rocky islet. After being cut off from the nearby shore, the islet operated as a seawall, causing the sea waves to [&hellip;]<\\\/p>\\n\",\"post_content\":\"The tombolo of St. Efthimia is located south of Lemnos, on the southwest shore of Cape \\\"Fakos\\\". The tombolo is a natural corridor composed of loose sediments that links the coast to the neighboring rocky islet.\\r\\n\\r\\nAfter being cut off from the nearby shore, the islet operated as a seawall, causing the sea waves to lose their carrying capacity and deposit the sediments they carried.\\r\\n\\r\\nThe land strip was formed over time by the constant deposition of sediment from the sea waves, and visitors may observe and stroll on it as well as visit the charming church of St. Efthimia.\",\"post_title\":\"St. Efthimia Tombolo\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/st-efthimia-tombolo\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"St. Efthimia Tombolo\\\" width=\\\"300\\\" height=\\\"210\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/13-\\u03a4\\u03cc\\u03bc\\u03c0\\u03bf\\u03bb\\u03bf-\\u0391\\u03b3\\u03af\\u03b1\\u03c2-\\u0395\\u03c5\\u03b8\\u03c5\\u03bc\\u03af\\u03b1\\u03c2-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.809040\",\"%wpcf-longtitude%\":\"25.141208\",\"%wpcf-location%\":\"\\u0391\\u03ba\\u03c1\\u03c9\\u03c4\\u03ae\\u03c1\\u03b9 \\u0391\\u03b3\\u03af\\u03b1\\u03c2 \\u0395\\u03c5\\u03b8\\u03c5\\u03bc\\u03af\\u03b1\\u03c2 (\\u03a3\\u03c4\\u03b1\\u03c5\\u03c1\\u03cc\\u03c2) \\u03a6\\u03b1\\u03ba\\u03cc\\u03c2\",\"%_wpgmp_metabox_latitude%\":\"39.809040\",\"%_wpgmp_metabox_longitude%\":\"25.141208\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"14\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi.png\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2760\",\"%_edit_lock%\":\"1655280669:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%84%cf%8c%ce%bc%cf%80%ce%bf%ce%bb%ce%bf-%ce%b1%ce%b3%ce%af%ce%b1%cf%82-%ce%b5%cf%85%ce%b8%cf%85%ce%bc%ce%af%ce%b1%cf%82\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/13-\\u03a4\\u03cc\\u03bc\\u03c0\\u03bf\\u03bb\\u03bf-\\u0391\\u03b3\\u03af\\u03b1\\u03c2-\\u0395\\u03c5\\u03b8\\u03c5\\u03bc\\u03af\\u03b1\\u03c2.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20318\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/13-\\u03a4\\u03cc\\u03bc\\u03c0\\u03bf\\u03bb\\u03bf-\\u0391\\u03b3\\u03af\\u03b1\\u03c2-\\u0395\\u03c5\\u03b8\\u03c5\\u03bc\\u03af\\u03b1\\u03c2.jpg, 13-\\u03a4\\u03cc\\u03bc\\u03c0\\u03bf\\u03bb\\u03bf \\u0391\\u03b3\\u03af\\u03b1\\u03c2 \\u0395\\u03c5\\u03b8\\u03c5\\u03bc\\u03af\\u03b1\\u03c2, \",\"%_et_pb_truncate_post%\":\"<p>The tombolo of St. Efthimia is located south of Lemnos, on the southwest shore of Cape &#8220;Fakos&#8221;. 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geosites\"},\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\"},\"id\":3588,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\",\"name\":\"\\u03a0\\u03b1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b9\\u03bf\\u03b9\",\"id\":\"14\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Pournias Erosion Formations\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Pournias Erosion Formations\\\" width=\\\"300\\\" height=\\\"164\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/26-\\u0391\\u03ba\\u03c1\\u03c9\\u03c4\\u03ae\\u03c1\\u03b9\\u03bf-\\u03a0\\u03bf\\u03c5\\u03c1\\u03bd\\u03b9\\u03ac-\\u03b3\\u03b5\\u03c9\\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2-\\u03b4\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-2-scaled-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/pournias-erosion-formations\\\/\\\">Pournias Erosion Formations<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/pournias-erosion-formations\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The impressive Pournias coastal erosion formations are visible in the thick layered sandstone and conglomerate rocks of northern Lemnos, west of Cape Pournia. The area is covered with sedimentary geological formations from Upper Eocene-Lower Oligocene deposited in underwater channels 27-33 million years ago. Honeycomb and spheroidal types of weathering have been observed in the area. [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.951\",\"lng\":\"25.287\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/pournias-erosion-formations\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The impressive Pournias coastal erosion formations are visible in the thick layered sandstone and conglomerate rocks of northern Lemnos, west of Cape Pournia. The area is covered with sedimentary geological formations from Upper Eocene-Lower Oligocene deposited in underwater channels 27-33 million years ago. Honeycomb and spheroidal types of weathering have been observed in the area. [&hellip;]<\\\/p>\\n\",\"post_content\":\"The impressive Pournias coastal erosion formations are visible in the thick layered sandstone and conglomerate rocks of northern Lemnos, west of Cape Pournia.\\r\\n\\r\\nThe area is covered with sedimentary geological formations from Upper Eocene-Lower Oligocene deposited in underwater channels 27-33 million years ago.\\r\\n\\r\\nHoneycomb and spheroidal types of weathering have been observed in the area. This is the result of the differential erosion of the sandstone rocks, caused by the structure of the rock which creates weak areas on its surface which are affected by sea waves and salt deposited by sea spray. This process results in impressive and complicated formations in the rocks.\",\"post_title\":\"Pournias Erosion Formations\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/pournias-erosion-formations\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Pournias Erosion Formations\\\" width=\\\"300\\\" height=\\\"164\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/26-\\u0391\\u03ba\\u03c1\\u03c9\\u03c4\\u03ae\\u03c1\\u03b9\\u03bf-\\u03a0\\u03bf\\u03c5\\u03c1\\u03bd\\u03b9\\u03ac-\\u03b3\\u03b5\\u03c9\\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2-\\u03b4\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-2-scaled-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.951\",\"%wpcf-longtitude%\":\"25.287\",\"%wpcf-location%\":\"\\u0391\\u03ba. \\u03a0\\u03bf\\u03c5\\u03c1\\u03bd\\u03b9\\u03ac\",\"%_wpgmp_metabox_latitude%\":\"39.951\",\"%_wpgmp_metabox_longitude%\":\"25.287\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"14\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi.png\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"3001\",\"%_edit_lock%\":\"1655281531:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%bc%ce%bf%cf%81%cf%86%ce%ad%cf%82-%ce%b4%ce%b9%ce%ac%ce%b2%cf%81%cf%89%cf%83%ce%b7%cf%82-%ce%b1%ce%ba%cf%81%cf%89%cf%84%ce%b7%cf%81%ce%af%ce%bf%cf%85-%cf%80%ce%bf%cf%85%cf%81%ce%bd%ce%b9%ce%ac\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/26-\\u0391\\u03ba\\u03c1\\u03c9\\u03c4\\u03ae\\u03c1\\u03b9\\u03bf-\\u03a0\\u03bf\\u03c5\\u03c1\\u03bd\\u03b9\\u03ac-\\u03b3\\u03b5\\u03c9\\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2-\\u03b4\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-2.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20359, 20360, 20361, 20362, 20363, 20364\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/pournias3.jpg, pournias3, \",\"%_et_pb_truncate_post%\":\"<p>The impressive Pournias coastal erosion formations are visible in the thick layered sandstone and conglomerate rocks of northern Lemnos, west of Cape Pournia.<\\\/p>\\n<p>The area is covered with sedimentary geological formations from Upper Eocene-Lower Oligocene deposited in underwater channels 27-33 million years ago.<\\\/p>\\n<p>Honeycomb and spheroidal types of weathering have been observed in the area. 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src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/5-\\u03a0\\u03b1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b9\\u03b5\\u03c2-\\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2-\\u03b4\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-\\u0391\\u03b3\\u03af\\u03bf\\u03c5-\\u0399\\u03c9\\u03ac\\u03bd\\u03bd\\u03b7-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/coastal-erosion-formations-of-st-ioannis\\\/\\\">Coastal Erosion Formations of St. Ioannis<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/coastal-erosion-formations-of-st-ioannis\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The coastal columnar formations (stacks) northwest of Kaspakas on the beach of Agios Ioannis are geoforms formed by the sea eroding pyroclastic formations caused by intense volcanic activity during the Lower Miocene. Coastal columns formations (stacks) refer to rock formations that rise above sea level along rocky beaches. They occur as a result of the [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9248\",\"lng\":\"25.0673676\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/coastal-erosion-formations-of-st-ioannis\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The coastal columnar formations (stacks) northwest of Kaspakas on the beach of Agios Ioannis are geoforms formed by the sea eroding pyroclastic formations caused by intense volcanic activity during the Lower Miocene. Coastal columns formations (stacks) refer to rock formations that rise above sea level along rocky beaches. They occur as a result of the [&hellip;]<\\\/p>\\n\",\"post_content\":\"<div class=\\\"sections__field-body\\\">\\r\\n\\r\\nThe coastal columnar formations (stacks) northwest of Kaspakas on the beach of Agios Ioannis are geoforms formed by the sea eroding pyroclastic formations caused by intense volcanic activity during the Lower Miocene.\\r\\n\\r\\nCoastal columns formations (stacks) refer to rock formations that rise above sea level along rocky beaches. They occur as a result of the strong differential erosion of a rocky beach by the sea waves and wind.\\r\\n\\r\\nThe definition \\\"stack\\\" is derived from the word \\\"stakkur\\\" which is the Scandinavian dialect of the Faeroe Islands, where these coastal formations are common along the high, steep, and rocky beaches.\\r\\n\\r\\n<\\\/div>\",\"post_title\":\"Coastal Erosion Formations of St. Ioannis\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/coastal-erosion-formations-of-st-ioannis\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Coastal Erosion Formations of St. Ioannis\\\" width=\\\"300\\\" height=\\\"209\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/5-\\u03a0\\u03b1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b9\\u03b5\\u03c2-\\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2-\\u03b4\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-\\u0391\\u03b3\\u03af\\u03bf\\u03c5-\\u0399\\u03c9\\u03ac\\u03bd\\u03bd\\u03b7-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.9248\",\"%wpcf-longtitude%\":\"25.0673676\",\"%wpcf-location%\":\"\\u039a\\u03ac\\u03c3\\u03c0\\u03b1\\u03ba\\u03b1\\u03c2, \\u0386\\u03b3\\u03b9\\u03bf\\u03c2 \\u0399\\u03c9\\u03ac\\u03bd\\u03bd\\u03b7\\u03c2\",\"%_wpgmp_metabox_latitude%\":\"39.9248\",\"%_wpgmp_metabox_longitude%\":\"25.0673676\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"14\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi.png\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2750\",\"%_edit_lock%\":\"1655283054:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%80%ce%b1%cf%81%ce%ac%ce%ba%cf%84%ce%b9%ce%b5%cf%82-%ce%b4%ce%bf%ce%bc%ce%ad%cf%82-%ce%b4%ce%b9%ce%ac%ce%b2%cf%81%cf%89%cf%83%ce%b7%cf%82-%ce%b1%ce%b3%ce%af%ce%bf%cf%85-%ce%b9%cf%89%ce%ac%ce%bd\",\"%wpcf-image-gallery%\":\"\",\"%_wpcf-image-gallery-sort-order%\":\"20402\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/5-\\u03a0\\u03b1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b9\\u03b5\\u03c2-\\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2-\\u03b4\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-\\u0391\\u03b3\\u03af\\u03bf\\u03c5-\\u0399\\u03c9\\u03ac\\u03bd\\u03bd\\u03b7.jpg, 5-\\u03a0\\u03b1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b9\\u03b5\\u03c2 \\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2 \\u03b4\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2 \\u0391\\u03b3\\u03af\\u03bf\\u03c5 \\u0399\\u03c9\\u03ac\\u03bd\\u03bd\\u03b7, \",\"%_et_pb_truncate_post%\":\"<p>The coastal columnar formations (stacks) northwest of Kaspakas on the beach of Agios Ioannis are geoforms formed by the sea eroding pyroclastic formations caused by intense volcanic activity during the Lower Miocene.<\\\/p>\\n<p>Coastal columns formations (stacks) refer to rock formations that rise above sea level along rocky beaches. 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geosites\"},\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\"},\"id\":3592,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\",\"name\":\"\\u03a0\\u03b1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b9\\u03bf\\u03b9\",\"id\":\"14\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Louri Beach Erosion Formations\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Louri Beach Erosion Formations\\\" width=\\\"300\\\" height=\\\"209\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/49-\\u03a0\\u03b1\\u03c1\\u03b1\\u03bb\\u03af\\u03b1-\\u039b\\u03bf\\u03c5\\u03c1\\u03af-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/louri-beach-erosion-formations\\\/\\\">Louri Beach Erosion Formations<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/louri-beach-erosion-formations\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Louri beach is located near of the southeastern coast of Lemnos, to the east of the town of Skandali and distinguished by an intense folding of 33 million-year-old sandstone rocks. The layers of sandstone rocks curve and create a 90-degree angle along the Louri beach. This curve is caused due to the shear stresses caused [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.795656\",\"lng\":\"25.350254\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/louri-beach-erosion-formations\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Louri beach is located near of the southeastern coast of Lemnos, to the east of the town of Skandali and distinguished by an intense folding of 33 million-year-old sandstone rocks. The layers of sandstone rocks curve and create a 90-degree angle along the Louri beach. This curve is caused due to the shear stresses caused [&hellip;]<\\\/p>\\n\",\"post_content\":\"<div class=\\\"sections__field-body\\\">\\r\\n<div class=\\\"sections__field-body\\\">\\r\\n\\r\\nLouri beach is located near of the southeastern coast of Lemnos, to the east of the town of Skandali and distinguished by an intense folding of 33 million-year-old sandstone rocks.\\r\\n\\r\\nThe layers of sandstone rocks curve and create a 90-degree angle along the Louri beach. This curve is caused due to the shear stresses caused by the activation of large faults.\\r\\n\\r\\nIn these sandstone layers can be found impressive honeycomb weathering shapes, formed by the wind, waves and sea spray.\\r\\n\\r\\nClose by there are also sand dunes formed by the deposition of products from the erosion of sandstone rocks.\\r\\n\\r\\n<\\\/div>\\r\\n<\\\/div>\",\"post_title\":\"Louri Beach Erosion Formations\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/louri-beach-erosion-formations\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Louri Beach Erosion Formations\\\" width=\\\"300\\\" height=\\\"209\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/49-\\u03a0\\u03b1\\u03c1\\u03b1\\u03bb\\u03af\\u03b1-\\u039b\\u03bf\\u03c5\\u03c1\\u03af-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.795656\",\"%wpcf-longtitude%\":\"25.350254\",\"%wpcf-location%\":\"\\u03a0\\u03b1\\u03c1\\u03b1\\u03bb\\u03af\\u03b1 \\u039b\\u03bf\\u03c5\\u03c1\\u03af\",\"%_wpgmp_metabox_latitude%\":\"39.795656\",\"%_wpgmp_metabox_longitude%\":\"25.350254\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"14\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi.png\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2735\",\"%_edit_lock%\":\"1655288061:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%80%ce%b1%cf%81%ce%b1%ce%bb%ce%af%ce%b1-%ce%bb%ce%bf%cf%85%cf%81%ce%af\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/49-\\u03a0\\u03b1\\u03c1\\u03b1\\u03bb\\u03af\\u03b1-\\u039b\\u03bf\\u03c5\\u03c1\\u03af.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20444\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/49-\\u03a0\\u03b1\\u03c1\\u03b1\\u03bb\\u03af\\u03b1-\\u039b\\u03bf\\u03c5\\u03c1\\u03af.jpg, 49-\\u03a0\\u03b1\\u03c1\\u03b1\\u03bb\\u03af\\u03b1 \\u039b\\u03bf\\u03c5\\u03c1\\u03af, \",\"%_et_pb_truncate_post%\":\"<p>Louri beach is located near of the southeastern coast of Lemnos, to the east of the town of Skandali and distinguished by an intense folding of 33 million-year-old sandstone rocks.<\\\/p>\\n<p>The layers of sandstone rocks curve and create a 90-degree angle along the Louri beach. 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geosites\"},\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\"},\"id\":3594,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\",\"name\":\"\\u03a0\\u03b1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b9\\u03bf\\u03b9\",\"id\":\"14\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"&#8220;Limnian Earth&#8221; mining site\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"&#8220;Limnian Earth&#8221; mining site\\\" width=\\\"300\\\" height=\\\"210\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/24-\\u039b\\u03b7\\u03bc\\u03bd\\u03af\\u03b1-\\u0393\\u03b7-\\u0391\\u03b3\\u03b9\\u03cc\\u03c7\\u03c9\\u03bc\\u03b1-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/limnian-earth-mining-site\\\/\\\">&#8220;Limnian Earth&#8221; mining site<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/limnian-earth-mining-site\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The ancient mining site of \\\"Limnian Earth\\\" is located between the villages of Kotsinas and Repanidi, on the hill of Mosichlos at the site \\\"Agiohoma\\\" (holy soil). The site is characterized by a reddish clay substance with a high iron and sulfur content that was widely used until the early twentieth century. First mentioned by [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.933\",\"lng\":\"25.286\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/limnian-earth-mining-site\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The ancient mining site of \\\"Limnian Earth\\\" is located between the villages of Kotsinas and Repanidi, on the hill of Mosichlos at the site \\\"Agiohoma\\\" (holy soil). The site is characterized by a reddish clay substance with a high iron and sulfur content that was widely used until the early twentieth century. First mentioned by [&hellip;]<\\\/p>\\n\",\"post_content\":\"<div class=\\\"sections__field-body\\\">\\r\\n\\r\\nThe ancient mining site of \\\"Limnian Earth\\\" is located between the villages of Kotsinas and Repanidi, on the hill of Mosichlos at the site \\\"Agiohoma\\\" (holy soil). The site is characterized by a reddish clay substance with a high iron and sulfur content that was widely used until the early twentieth century.\\r\\n\\r\\nFirst mentioned by Herodotus, the healing abilities of the \\\"Limnian Earth\\\" are mythologically connected with Hephaestus whose wounds were healed by them following his expulsion from Olympus. 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Tufa is generally found on the shoreline of the Hephaistia archeological site. These are deposits made up of porous limestone sandstone mosaic, and lattice that include fragments of the underlying molassic formation. The multitude of shells in the shallow water is characteristic [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9688561\",\"lng\":\"25.3281717\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/hephaistia-quarry\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The ancient tufa quarry is located northeast of the ancient theater of Hephaistia. Tufa is generally found on the shoreline of the Hephaistia archeological site. These are deposits made up of porous limestone sandstone mosaic, and lattice that include fragments of the underlying molassic formation. The multitude of shells in the shallow water is characteristic [&hellip;]<\\\/p>\\n\",\"post_content\":\"The ancient tufa quarry is located northeast of the ancient theater of Hephaistia.\\r\\n\\r\\nTufa is generally found on the shoreline of the Hephaistia archeological site. These are deposits made up of porous limestone sandstone mosaic, and lattice that include fragments of the underlying molassic formation. The multitude of shells in the shallow water is characteristic of these Pleistocene deposits. The deposits, having accumulated on the underlying molassic rocks, have a thickness of more than 50m in certain locations.\\r\\n\\r\\nHephaistias' open ancient quarry once operated in the coastal region. The enormity of the site shows the scale of the mining. 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geosites\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/geoarchaeology_result-small.png\"},\"id\":3602,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/geoarchaeology_result-small.png\",\"name\":\"\\u0391\\u03bd\\u03b8\\u03c1\\u03c9\\u03c0\\u03bf\\u03b3\\u03b5\\u03bd\\u03b5\\u03af\\u03c2\",\"id\":\"2\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Cape Pournias Quarry\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Cape Pournias Quarry\\\" width=\\\"300\\\" height=\\\"200\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/25-\\u039b\\u03b1\\u03c4\\u03bf\\u03bc\\u03b5\\u03af\\u03bf-\\u03b1\\u03ba\\u03c1\\u03c9\\u03c4\\u03b7\\u03c1\\u03af\\u03bf\\u03c5-\\u03a0\\u03bf\\u03c5\\u03c1\\u03bd\\u03b9\\u03ac-scaled-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-pournias-quarry\\\/\\\">Cape Pournias Quarry<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-pournias-quarry\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>There are several tufa formations towards the end of Cape Pournias. These are deposits made up of porous limestone sandstone mosaic, as well as lattice that include fragments of the molassic formation. Many shells, characteristic of the shallow water, may be found in these Pleistocene deposits. The deposits which have been accumulated on the underlying [&hellip;]<\\\/p>\\n\",\"address\":\"X73Q+6H \\u0391\\u03c4\\u03c3\\u03b9\\u03ba\\u03ae, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.95330501587282\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.28883540608215\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-pournias-quarry\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>There are several tufa formations towards the end of Cape Pournias. These are deposits made up of porous limestone sandstone mosaic, as well as lattice that include fragments of the molassic formation. Many shells, characteristic of the shallow water, may be found in these Pleistocene deposits. The deposits which have been accumulated on the underlying [&hellip;]<\\\/p>\\n\",\"post_content\":\"There are several tufa formations towards the end of Cape Pournias. These are deposits made up of porous limestone sandstone mosaic, as well as lattice that include fragments of the molassic formation. Many shells, characteristic of the shallow water, may be found in these Pleistocene deposits. The deposits which have been accumulated on the underlying molassic rocks have a thickness of more than 50m in certain locations.\\r\\n\\r\\nAn open quarry operated in this place and the scale of the site reflects the extent of the operation since it covers the majority of Cape Pournia.\\r\\n\\r\\nArchitectural remains built of tufa have been discovered on the opposite side of the quarry of Pournia, near the archeological site of the temple of Kaviria. 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These are deposits made up of porous limestone sandstone mosaic, as well as lattice that include fragments of the molassic formation. Many shells, characteristic of the shallow water, may be found in these Pleistocene deposits. The deposits which have been accumulated on the underlying molassic rocks have a thickness of more than 50m in certain locations.<\\\/p>\\n<p>An open quarry operated in this place and the scale of the site reflects the extent of the operation since it covers the majority of Cape Pournia.<\\\/p>\\n<p>Architectural remains built of tufa have been discovered on the opposite side of the quarry of Pournia, near the archeological site of the temple of Kaviria. 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geosites\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/geoarchaeology_result-small.png\"},\"id\":3604,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/geoarchaeology_result-small.png\",\"name\":\"\\u0391\\u03bd\\u03b8\\u03c1\\u03c9\\u03c0\\u03bf\\u03b3\\u03b5\\u03bd\\u03b5\\u03af\\u03c2\",\"id\":\"2\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Asprolimni\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Asprolimni\\\" width=\\\"300\\\" height=\\\"209\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/39-\\u0391\\u03c3\\u03c0\\u03c1\\u03bf\\u03bb\\u03af\\u03bc\\u03bd\\u03b7-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/asprolimni\\\/\\\">Asprolimni<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/asprolimni\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Lemnos' Asprolimni (meaning \\u201cWhite Lake\\u201d) is located in the eastern section of the island, between the lakes Hortarolimni and the Salt pan. It covers around 500 acres and is part of the NATURA 2000 conservation network since it is home to a great number of rare and endangered species. A saltwater lake only open during [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.931187\",\"lng\":\"25.380258\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/asprolimni\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Lemnos' Asprolimni (meaning \\u201cWhite Lake\\u201d) is located in the eastern section of the island, between the lakes Hortarolimni and the Salt pan. It covers around 500 acres and is part of the NATURA 2000 conservation network since it is home to a great number of rare and endangered species. A saltwater lake only open during [&hellip;]<\\\/p>\\n\",\"post_content\":\"Lemnos' Asprolimni (meaning \\u201cWhite Lake\\u201d) is located in the eastern section of the island, between the lakes Hortarolimni and the Salt pan. It covers around 500 acres and is part of the NATURA 2000 conservation network since it is home to a great number of rare and endangered species.\\r\\n\\r\\nA saltwater lake only open during the summer, Asprolimni earned its name from the \\u00a0thick coating of salt on its dried bottom \\u00a0throughout the summer months.\\r\\n\\r\\nThe strong NE winds that blow on the coast of Keros carry the materials of the area's sedimentary rocks at high speeds and deposit them in the\\u00a0area of Asprolimni, generating successive sand dunes. Visitors to Asprolimni may see a variety of wild geese, herons, kingfishers, copperpoxes, and even dense flocks of pink flamingos, who stop in the area to feed and rest.\",\"post_title\":\"Asprolimni\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/asprolimni\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Asprolimni\\\" width=\\\"300\\\" height=\\\"209\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/39-\\u0391\\u03c3\\u03c0\\u03c1\\u03bf\\u03bb\\u03af\\u03bc\\u03bd\\u03b7-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.931187\",\"%wpcf-longtitude%\":\"25.380258\",\"%wpcf-location%\":\"\\u0391\\u03bb\\u03c5\\u03ba\\u03ae\",\"%_wpgmp_metabox_latitude%\":\"39.931187\",\"%_wpgmp_metabox_longitude%\":\"25.380258\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:2:{i:0;s:1:\\\"6\\\";i:1;s:2:\\\"15\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/waters.png\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2745\",\"%_edit_lock%\":\"1657091617:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%b1%cf%83%cf%80%cf%81%ce%bf%ce%bb%ce%af%ce%bc%ce%bd%ce%b7\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/39-\\u0391\\u03c3\\u03c0\\u03c1\\u03bf\\u03bb\\u03af\\u03bc\\u03bd\\u03b7.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20635\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/39-\\u0391\\u03c3\\u03c0\\u03c1\\u03bf\\u03bb\\u03af\\u03bc\\u03bd\\u03b7.jpg, 39-\\u0391\\u03c3\\u03c0\\u03c1\\u03bf\\u03bb\\u03af\\u03bc\\u03bd\\u03b7, \",\"%_et_pb_truncate_post%\":\"<p>Lemnos&#8217; Asprolimni (meaning \\u201cWhite Lake\\u201d) is located in the eastern section of the island, between the lakes Hortarolimni and the Salt pan. It covers around 500 acres and is part of the NATURA 2000 conservation network since it is home to a great number of rare and endangered species.<\\\/p>\\n<p>A saltwater lake only open during the summer, Asprolimni earned its name from the \\u00a0thick coating of salt on its dried bottom \\u00a0throughout the summer months.<\\\/p>\\n<p>The strong NE winds that blow on the coast of Keros carry the materials of the area&#8217;s sedimentary rocks at high speeds and deposit them in the\\u00a0area of Asprolimni, generating successive sand dunes. 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systems\"},\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/apothesis_sm-small.png\"},\"id\":3611,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/waters_result-small.png\",\"name\":\"\\u03a5\\u03b4\\u03b1\\u03c4\\u03b9\\u03ba\\u03ac \\u03c3\\u03c5\\u03c3\\u03c4\\u03ae\\u03bc\\u03b1\\u03c4\\u03b1\",\"id\":\"6\",\"type\":\"category\"},{\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/apothesis_sm-small.png\",\"name\":\"\\u0391\\u03b9\\u03bf\\u03bb\\u03b9\\u03ba\\u03bf\\u03af\",\"id\":\"15\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Chortarolimni\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Chortarolimni\\\" width=\\\"300\\\" height=\\\"209\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/41-\\u03a7\\u03bf\\u03c1\\u03c4\\u03b1\\u03c1\\u03bf\\u03bb\\u03af\\u03bc\\u03bd\\u03b7-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/chortarolimni\\\/\\\">Chortarolimni<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/chortarolimni\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The southernmost of three significant wetlands, Chortarolimni is located in the eastern section of Lemnos near the settlement of Roussopouli. Chortarolimni is a 2,300-acre seasonal saltwater wetland in the Mediterranean. Together with the Salt pan and Asprolimni, it is a significant wetland for a variety of rare and endangered animals and plants, and is part [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.89354\",\"lng\":\"25.34147\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/chortarolimni\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The southernmost of three significant wetlands, Chortarolimni is located in the eastern section of Lemnos near the settlement of Roussopouli. Chortarolimni is a 2,300-acre seasonal saltwater wetland in the Mediterranean. Together with the Salt pan and Asprolimni, it is a significant wetland for a variety of rare and endangered animals and plants, and is part [&hellip;]<\\\/p>\\n\",\"post_content\":\"<div class=\\\"sections__field-body\\\">\\r\\n\\r\\nThe southernmost of three significant wetlands, Chortarolimni is located in the eastern section of Lemnos near the settlement of Roussopouli.\\r\\n\\r\\nChortarolimni is a 2,300-acre seasonal saltwater wetland in the Mediterranean. Together with the Salt pan and Asprolimni, it is a significant wetland for a variety of rare and endangered animals and plants, and is part of the Natura 2000 network.\\r\\n\\r\\nThe waters of Chortarolimni are brackish and during the summer months Chortarolimni dries up. The area around the lake consists of sand dunes whose width approaches 1000 meters while their thickness is about 5 meters.\\r\\n\\r\\nSeveral plant species may be found in Chortarolimni, including rush (<em>Juncus <\\\/em>spp.), freshwater-common reed (<em>Phragmites australis<\\\/em>), bulrush (<em>Scirpus<\\\/em> spp.), arthrocnemum (<em>Arthrocnemum<\\\/em> spp.), and marram grass (<em>Ammophila arenaria<\\\/em>).\\r\\n\\r\\nThe Chortarolimni wetland is an important geographical feature of the area since it serves as a resting and feeding ground for many rare bird migrational species. In addition to the famed pink flamingo, visitors to the region may see other bird species such as the Lesser kestrel (<em>Falcon naumanni<\\\/em>), Marsh Harrier (<em>Circus aeruginosus)<\\\/em>, Hen harrier (<em>Circus cyaneus<\\\/em>), and others.\\r\\n\\r\\n<\\\/div>\",\"post_title\":\"Chortarolimni\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/chortarolimni\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Chortarolimni\\\" width=\\\"300\\\" height=\\\"209\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/41-\\u03a7\\u03bf\\u03c1\\u03c4\\u03b1\\u03c1\\u03bf\\u03bb\\u03af\\u03bc\\u03bd\\u03b7-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.89354\",\"%wpcf-longtitude%\":\"25.34147\",\"%_wpgmp_metabox_latitude%\":\"39.89354\",\"%_wpgmp_metabox_longitude%\":\"25.34147\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:2:{i:0;s:1:\\\"6\\\";i:1;s:2:\\\"15\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/waters.png\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-location%\":\"\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2779\",\"%_edit_lock%\":\"1657097833:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%87%ce%bf%cf%81%cf%84%ce%b1%cf%81%ce%bf%ce%bb%ce%af%ce%bc%ce%bd%ce%b7\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/41-\\u03a7\\u03bf\\u03c1\\u03c4\\u03b1\\u03c1\\u03bf\\u03bb\\u03af\\u03bc\\u03bd\\u03b7.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20675\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/41-\\u03a7\\u03bf\\u03c1\\u03c4\\u03b1\\u03c1\\u03bf\\u03bb\\u03af\\u03bc\\u03bd\\u03b7.jpg, 41-\\u03a7\\u03bf\\u03c1\\u03c4\\u03b1\\u03c1\\u03bf\\u03bb\\u03af\\u03bc\\u03bd\\u03b7, \",\"%_et_pb_truncate_post%\":\"<p>The southernmost of three significant wetlands, Chortarolimni is located in the eastern section of Lemnos near the settlement of Roussopouli.<\\\/p>\\n<p>Chortarolimni is a 2,300-acre seasonal saltwater wetland in the Mediterranean. Together with the Salt pan and Asprolimni, it is a significant wetland for a variety of rare and endangered animals and plants, and is part of the Natura 2000 network.<\\\/p>\\n<p>The waters of Chortarolimni are brackish and during the summer months Chortarolimni dries up. The area around the lake consists of sand dunes whose width approaches 1000 meters while their thickness is about 5 meters.<\\\/p>\\n<p>Several plant species may be found in Chortarolimni, including rush (Juncus spp.), freshwater-common reed (Phragmites australis), bulrush (Scirpus spp.), arthrocnemum (Arthrocnemum spp.), and marram grass (Ammophila arenaria).<\\\/p>\\n<p>The Chortarolimni wetland is an important geographical feature of the area since it serves as a resting and feeding ground for many rare bird migrational species. 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systems\"},\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/apothesis_sm-small.png\"},\"id\":3613,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/waters_result-small.png\",\"name\":\"\\u03a5\\u03b4\\u03b1\\u03c4\\u03b9\\u03ba\\u03ac \\u03c3\\u03c5\\u03c3\\u03c4\\u03ae\\u03bc\\u03b1\\u03c4\\u03b1\",\"id\":\"6\",\"type\":\"category\"},{\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/apothesis_sm-small.png\",\"name\":\"\\u0391\\u03b9\\u03bf\\u03bb\\u03b9\\u03ba\\u03bf\\u03af\",\"id\":\"15\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Katsaitis Waterfall\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Katsaitis Waterfall\\\" width=\\\"300\\\" height=\\\"209\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/3-\\u039a\\u03b1\\u03c4\\u03b1\\u03c1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b7\\u03c2-\\u039a\\u03b1\\u03c4\\u03c3\\u03b1\\u0390\\u03c4\\u03b7-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/katsaitis-waterfall\\\/\\\">Katsaitis Waterfall<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/katsaitis-waterfall\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The impressive Katsaitis waterfall is found north of St. Ioannis, where the Katsaitis stream crosses the 33-million-year-old sandstone rocks of Lemnos. The waterfall is formed by the discontinuities in the rocks caused by the movement of the Kaspakas active fault. The basin at the foot of the waterfall was formed due to the force of [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.938\",\"lng\":\"25.066\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/katsaitis-waterfall\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The impressive Katsaitis waterfall is found north of St. Ioannis, where the Katsaitis stream crosses the 33-million-year-old sandstone rocks of Lemnos. The waterfall is formed by the discontinuities in the rocks caused by the movement of the Kaspakas active fault. The basin at the foot of the waterfall was formed due to the force of [&hellip;]<\\\/p>\\n\",\"post_content\":\"<div class=\\\"sections__field-body\\\">\\r\\n\\r\\nThe impressive Katsaitis waterfall is found north of St. Ioannis, where the Katsaitis stream crosses the 33-million-year-old sandstone rocks of Lemnos.\\r\\n\\r\\nThe waterfall is formed by the discontinuities in the rocks caused by the movement of the Kaspakas active fault. The basin at the foot of the waterfall was formed due to the force of the falling water, which resulted in the subsiding of ground material, forming the natural plunge pool.\\r\\n\\r\\nAt the point on either side of the waterfall and the observer, the impressive alternation of geological formations is displayed. This was made by the activity of Kaspakas fault which brought the sedimentary rock of Lemnos into contact with newer volcanic rocks through multiple seismic sequences.\\r\\n\\r\\n<\\\/div>\",\"post_title\":\"Katsaitis Waterfall\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/katsaitis-waterfall\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Katsaitis Waterfall\\\" width=\\\"300\\\" height=\\\"209\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/3-\\u039a\\u03b1\\u03c4\\u03b1\\u03c1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b7\\u03c2-\\u039a\\u03b1\\u03c4\\u03c3\\u03b1\\u0390\\u03c4\\u03b7-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.938\",\"%wpcf-longtitude%\":\"25.066\",\"%wpcf-location%\":\"\\u039a\\u03b1\\u03c4\\u03c3\\u03b1\\u0390\\u03c4\\u03b7\\u03c2, \\u039a\\u03ac\\u03c3\\u03c0\\u03b1\\u03ba\\u03b1\\u03c2\",\"%_wpgmp_metabox_latitude%\":\"39.938\",\"%_wpgmp_metabox_longitude%\":\"25.066\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"6\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/tectonic.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2752\",\"%_edit_lock%\":\"1657099942:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%ba%ce%b1%cf%84%ce%b1%cf%81%cf%81%ce%ac%ce%ba%cf%84%ce%b7%cf%82-%ce%ba%ce%b1%cf%84%cf%83%ce%b1%ce%90%cf%84%ce%b7\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/3-\\u039a\\u03b1\\u03c4\\u03b1\\u03c1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b7\\u03c2-\\u039a\\u03b1\\u03c4\\u03c3\\u03b1\\u0390\\u03c4\\u03b7.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20718\",\"%wpcf-code%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/3-\\u039a\\u03b1\\u03c4\\u03b1\\u03c1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b7\\u03c2-\\u039a\\u03b1\\u03c4\\u03c3\\u03b1\\u0390\\u03c4\\u03b7.jpg, 3-\\u039a\\u03b1\\u03c4\\u03b1\\u03c1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b7\\u03c2 \\u039a\\u03b1\\u03c4\\u03c3\\u03b1\\u0390\\u03c4\\u03b7, \",\"%_et_pb_truncate_post%\":\"<p>The impressive Katsaitis waterfall is found north of St. Ioannis, where the Katsaitis stream crosses the 33-million-year-old sandstone rocks of Lemnos.<\\\/p>\\n<p>The waterfall is formed by the discontinuities in the rocks caused by the movement of the Kaspakas active fault. 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src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/31-\\u0391\\u03bd\\u03b1\\u03b3\\u03ad\\u03bd\\u03bd\\u03b7\\u03c3\\u03b7-\\u03c5\\u03b4\\u03c1\\u03bf\\u03b3\\u03c1\\u03b1\\u03c6\\u03b9\\u03ba\\u03bf\\u03cd-\\u03b4\\u03b9\\u03ba\\u03c4\\u03cd\\u03bf\\u03c5-\\u039d\\u03b5\\u03c6\\u03c4\\u03af\\u03bd\\u03b1\\u03c2-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/regeneration-of-neftinas-hydrographic-network\\\/\\\">Regeneration of Neftina\\u2019s Hydrographic Network<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/regeneration-of-neftinas-hydrographic-network\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Going up the road to the Church of Kaveira near the cape of Chloe in NE Lemnos, the Neftina valley can be seen on its right-hand side. Deep ravines can be observed in the valley\\u2019s hydrographic network, phenomena classified as the regeneration of the hydrographic network. These phenomena are caused by the activity of the [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.980\",\"lng\":\"25.354\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/regeneration-of-neftinas-hydrographic-network\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Going up the road to the Church of Kaveira near the cape of Chloe in NE Lemnos, the Neftina valley can be seen on its right-hand side. Deep ravines can be observed in the valley\\u2019s hydrographic network, phenomena classified as the regeneration of the hydrographic network. These phenomena are caused by the activity of the [&hellip;]<\\\/p>\\n\",\"post_content\":\"Going up the road to the Church of Kaveira near the cape of Chloe in NE Lemnos, the Neftina valley can be seen on its right-hand side.\\r\\n\\r\\nDeep ravines can be observed in the valley\\u2019s hydrographic network, phenomena classified as the regeneration of the hydrographic network. These phenomena are caused by the activity of the Neftina active fault, which caused the northern portion of the valley to sink and the southern part to rise.\\r\\n\\r\\nThe Neftina NW-SE\\u00a0fault affects the hydrographic network by elevating the plateau, which is a landscape\\u00a0with moderate slopes, to the\\u00a0point where the hydrographic network has lost its transport capacity. \\u00a0As a result, the water begins a new cycle of erosion, eroding the\\u00a0terrain\\u00a0deeper and deeper\\u00a0until it reaches the new basic level of the riverbed, resulting in this impressive formation in the landscape.\",\"post_title\":\"Regeneration of Neftina\\u2019s Hydrographic Network\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/regeneration-of-neftinas-hydrographic-network\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Regeneration of Neftina\\u2019s Hydrographic Network\\\" width=\\\"300\\\" height=\\\"224\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/31-\\u0391\\u03bd\\u03b1\\u03b3\\u03ad\\u03bd\\u03bd\\u03b7\\u03c3\\u03b7-\\u03c5\\u03b4\\u03c1\\u03bf\\u03b3\\u03c1\\u03b1\\u03c6\\u03b9\\u03ba\\u03bf\\u03cd-\\u03b4\\u03b9\\u03ba\\u03c4\\u03cd\\u03bf\\u03c5-\\u039d\\u03b5\\u03c6\\u03c4\\u03af\\u03bd\\u03b1\\u03c2-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.980\",\"%wpcf-longtitude%\":\"25.354\",\"%wpcf-location%\":\"\\u0394\\u03c1\\u03cc\\u03bc\\u03bf\\u03c2 \\u03c0\\u03c1\\u03bf\\u03c2 \\u039d\\u03b5\\u03c6\\u03c4\\u03af\\u03bd\\u03b1 \\u03b1\\u03c0\\u03cc \\u039a\\u03b1\\u03b2\\u03b5\\u03af\\u03c1\\u03b9\\u03b1\",\"%_wpgmp_metabox_latitude%\":\"39.980\",\"%_wpgmp_metabox_longitude%\":\"25.354\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"6\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/waters.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2778\",\"%_edit_lock%\":\"1657104197:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%b1%ce%bd%ce%b1%ce%b3%ce%ad%ce%bd%ce%bd%ce%b7%cf%83%ce%b7-%cf%85%ce%b4%cf%81%ce%bf%ce%b3%cf%81%ce%b1%cf%86%ce%b9%ce%ba%ce%bf%cf%8d-%ce%b4%ce%b9%ce%ba%cf%84%cf%8d%ce%bf%cf%85-%ce%bd%ce%b5%cf%86\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/31-\\u0391\\u03bd\\u03b1\\u03b3\\u03ad\\u03bd\\u03bd\\u03b7\\u03c3\\u03b7-\\u03c5\\u03b4\\u03c1\\u03bf\\u03b3\\u03c1\\u03b1\\u03c6\\u03b9\\u03ba\\u03bf\\u03cd-\\u03b4\\u03b9\\u03ba\\u03c4\\u03cd\\u03bf\\u03c5-\\u039d\\u03b5\\u03c6\\u03c4\\u03af\\u03bd\\u03b1\\u03c2.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20757, 20758, 20759, 20760\",\"%wpcf-code%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/DJI_0810-scaled.jpg, DCIM100MEDIADJI_0810.JPG, DCIM100MEDIADJI_0810.JPG\",\"%_et_pb_truncate_post%\":\"<p>Going up the road to the Church of Kaveira near the cape of Chloe in NE Lemnos, the Neftina valley can be seen on its right-hand side.<\\\/p>\\n<p>Deep ravines can be observed in the valley\\u2019s hydrographic network, phenomena classified as the regeneration of the hydrographic network. 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systems\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/waters_result-small.png\"},\"id\":3618,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/waters_result-small.png\",\"name\":\"\\u03a5\\u03b4\\u03b1\\u03c4\\u03b9\\u03ba\\u03ac \\u03c3\\u03c5\\u03c3\\u03c4\\u03ae\\u03bc\\u03b1\\u03c4\\u03b1\",\"id\":\"6\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Gomati Beach Sand Dunes\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Gomati Beach Sand Dunes\\\" width=\\\"300\\\" height=\\\"169\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/22-\\u03a0\\u03b1\\u03c1\\u03b1\\u03bb\\u03af\\u03b1-\\u0393\\u03bf\\u03bc\\u03ac\\u03c4\\u03b9-2-scaled-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/gomati-beach-sand-dunes\\\/\\\">Gomati Beach Sand Dunes<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/gomati-beach-sand-dunes\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The Gomati beach, located on the northwest coast of Lemnos, north of the town of Katalakkos, is home to the impressive Gomati sand dunes. Large prominent sand hills in\\u00a0the surrounding\\u00a0landscape, these sand dunes are formed by wind erosion and the deposition of materials\\u00a0in the area. Strong NE winds transport the erosion materials from the area's [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.991804\",\"lng\":\"25.142415\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/gomati-beach-sand-dunes\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The Gomati beach, located on the northwest coast of Lemnos, north of the town of Katalakkos, is home to the impressive Gomati sand dunes. Large prominent sand hills in\\u00a0the surrounding\\u00a0landscape, these sand dunes are formed by wind erosion and the deposition of materials\\u00a0in the area. Strong NE winds transport the erosion materials from the area's [&hellip;]<\\\/p>\\n\",\"post_content\":\"<div class=\\\"sections__field-body\\\">\\r\\n\\r\\nThe Gomati beach, located on the northwest coast of Lemnos, north of the town of Katalakkos, is home to the impressive Gomati sand dunes. Large prominent sand hills in\\u00a0the surrounding\\u00a0landscape, these sand dunes are formed by wind erosion and the deposition of materials\\u00a0in the area.\\r\\n\\r\\nStrong NE winds transport the erosion materials from the area's tertiary sedimentary rocks, actively contributing to their creation. Because dune systems are dynamic and changing, the presence of vegetation is critical in holding down sand and preserving it\\u00a0from further\\u00a0erosion.\\r\\n\\r\\nThe Gomati Sand Dunes cover a large area along the coastline, enough to evoke the feeling of a miniature desert, and an unusual and unexpected scene for visitors to a Greek island.\\r\\n\\r\\n<\\\/div>\",\"post_title\":\"Gomati Beach Sand Dunes\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/gomati-beach-sand-dunes\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Gomati Beach Sand Dunes\\\" width=\\\"300\\\" height=\\\"169\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/22-\\u03a0\\u03b1\\u03c1\\u03b1\\u03bb\\u03af\\u03b1-\\u0393\\u03bf\\u03bc\\u03ac\\u03c4\\u03b9-2-scaled-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.991804\",\"%wpcf-longtitude%\":\"25.142415\",\"%wpcf-location%\":\"\\u03a0\\u03b1\\u03c1\\u03b1\\u03bb\\u03af\\u03b1 \\u0393\\u03bf\\u03bc\\u03b1\\u03c4\\u03af\\u03bf\\u03c5\",\"%_wpgmp_metabox_latitude%\":\"39.991804\",\"%_wpgmp_metabox_longitude%\":\"25.142415\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"15\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/apothesis.png\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"3049\",\"%_edit_lock%\":\"1657108538:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%80%ce%b1%cf%81%ce%b1%ce%bb%ce%af%ce%b1-%ce%b3%ce%bf%ce%bc%ce%ac%cf%84%ce%b9\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/22-\\u03a0\\u03b1\\u03c1\\u03b1\\u03bb\\u03af\\u03b1-\\u0393\\u03bf\\u03bc\\u03ac\\u03c4\\u03b9-2.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20820\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/22-\\u03a0\\u03b1\\u03c1\\u03b1\\u03bb\\u03af\\u03b1-\\u0393\\u03bf\\u03bc\\u03ac\\u03c4\\u03b9-2-scaled.jpg, 22-\\u03a0\\u03b1\\u03c1\\u03b1\\u03bb\\u03af\\u03b1 \\u0393\\u03bf\\u03bc\\u03ac\\u03c4\\u03b9 2, \",\"%_et_pb_truncate_post%\":\"<p>The Gomati beach, located on the northwest coast of Lemnos, north of the town of Katalakkos, is home to the impressive Gomati sand dunes. 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deposits\"},\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/apothesis_sm-small.png\"},\"id\":3624,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/apothesis_sm-small.png\",\"name\":\"\\u0391\\u03b9\\u03bf\\u03bb\\u03b9\\u03ba\\u03bf\\u03af\",\"id\":\"15\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Neftina Sand Dunes\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Neftina Sand Dunes\\\" width=\\\"300\\\" height=\\\"210\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/33-\\u039d\\u03b5\\u03c6\\u03c4\\u03af\\u03bd\\u03b1-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding 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The impressive dunes that characterize the local area were formed by the erosion of Oligocene sedimentary rocks. The continuous high-speed wind that transports the products of sandstone rock erosion contributes to their formation. The presence of vegetation actively helps [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.98348\",\"lng\":\"25.34951\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/neftina-sand-dunes\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The Neftina Sand Dunes are located in northeastern Lemnos, northeast of the archaeological site of Kaveri. The impressive dunes that characterize the local area were formed by the erosion of Oligocene sedimentary rocks. The continuous high-speed wind that transports the products of sandstone rock erosion contributes to their formation. The presence of vegetation actively helps [&hellip;]<\\\/p>\\n\",\"post_content\":\"<div class=\\\"sections__field-body\\\">\\r\\n\\r\\nThe Neftina Sand Dunes are located in northeastern Lemnos, northeast of the archaeological site of Kaveri. The impressive dunes that characterize the local area were formed by the erosion of Oligocene sedimentary rocks.\\r\\n\\r\\nThe continuous high-speed wind that transports the products of sandstone rock erosion contributes to their formation. 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deposits\"},\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/apothesis_sm-small.png\"},\"id\":3628,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/apothesis_sm-small.png\",\"name\":\"\\u0391\\u03b9\\u03bf\\u03bb\\u03b9\\u03ba\\u03bf\\u03af\",\"id\":\"15\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Avlona Gorge\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Avlona Gorge\\\" width=\\\"300\\\" height=\\\"227\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/20-\\u03a6\\u03b1\\u03c1\\u03ac\\u03b3\\u03b3\\u03b9-\\u0391\\u03c5\\u03bb\\u03ce\\u03bd\\u03b1-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/avlona-gorge\\\/\\\">Avlona Gorge<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/avlona-gorge\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The stream of the Avlona Gorge, found to the west of the Kornos village, makes its way through the sedimentary rocks and runs into the sea on a beach north of Myrina. The Avlona Gorge was formed in the area\\u2019s sedimentary rocks of sandstone and siltstone alternations about 33 million years old. A normal fault [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.921\",\"lng\":\"25.115\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/avlona-gorge\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The stream of the Avlona Gorge, found to the west of the Kornos village, makes its way through the sedimentary rocks and runs into the sea on a beach north of Myrina. The Avlona Gorge was formed in the area\\u2019s sedimentary rocks of sandstone and siltstone alternations about 33 million years old. A normal fault [&hellip;]<\\\/p>\\n\",\"post_content\":\"<div class=\\\"sections__field-body\\\">\\r\\n\\r\\nThe stream of the Avlona Gorge, found to the west of the Kornos village, makes its way through the sedimentary rocks and runs into the sea on a beach north of Myrina.\\r\\n\\r\\nThe Avlona Gorge was formed in the area\\u2019s sedimentary rocks of sandstone and siltstone alternations about 33 million years old. A normal fault with NE-SW orientation runs parallel to the stream bed displacing the sandstone rocks and resulting in a small waterfall.\\r\\n\\r\\n<\\\/div>\",\"post_title\":\"Avlona Gorge\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/avlona-gorge\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Avlona Gorge\\\" width=\\\"300\\\" height=\\\"227\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/20-\\u03a6\\u03b1\\u03c1\\u03ac\\u03b3\\u03b3\\u03b9-\\u0391\\u03c5\\u03bb\\u03ce\\u03bd\\u03b1-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.921\",\"%wpcf-longtitude%\":\"25.115\",\"%wpcf-location%\":\"\\u0386\\u03b3\\u03b9\\u03bf\\u03c2 \\u0399\\u03c9\\u03ac\\u03bd\\u03bd\\u03b7\\u03c2\",\"%_wpgmp_metabox_latitude%\":\"39.921\",\"%_wpgmp_metabox_longitude%\":\"25.115\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"3\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/geoforms.png\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2767\",\"%_edit_lock%\":\"1657781692:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%86%ce%b1%cf%81%ce%ac%ce%b3%ce%b3%ce%b9-%ce%b1%cf%8d%ce%bb%cf%89%ce%bd%ce%b1\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/20-\\u03a6\\u03b1\\u03c1\\u03ac\\u03b3\\u03b3\\u03b9-\\u0391\\u03c5\\u03bb\\u03ce\\u03bd\\u03b1.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20953\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/20-\\u03a6\\u03b1\\u03c1\\u03ac\\u03b3\\u03b3\\u03b9-\\u0391\\u03c5\\u03bb\\u03ce\\u03bd\\u03b1.jpg, 20-\\u03a6\\u03b1\\u03c1\\u03ac\\u03b3\\u03b3\\u03b9 \\u0391\\u03c5\\u03bb\\u03ce\\u03bd\\u03b1, \",\"%_et_pb_truncate_post%\":\"<p>The stream of the Avlona Gorge, found to the west of the Kornos village, makes its way through the sedimentary rocks and runs into the sea on a beach north of Myrina.<\\\/p>\\n<p>The Avlona Gorge was formed in the area\\u2019s sedimentary rocks of sandstone and siltstone alternations about 33 million years old. 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\\u2013 Erosion geoforms\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/geoforms_result-small.png\"},\"id\":3634,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/geoforms_result-small.png\",\"name\":\"\\u0393\\u03b5\\u03c9\\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2 \\u0391\\u03c0\\u03bf\\u03c3\\u03ac\\u03b8\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-\\u0394\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2\",\"id\":\"3\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Tafoni \\u2013 Mushroom weathering formation of St. Ioannis\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Tafoni \\u2013 Mushroom weathering formation of St. Ioannis\\\" width=\\\"300\\\" height=\\\"226\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/6-\\u03a4\\u03b1\\u03c6\\u03cc\\u03bd\\u03b9-\\u0391\\u03b3\\u03af\\u03bf\\u03c5-\\u0399\\u03c9\\u03ac\\u03bd\\u03bd\\u03b7-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/tafoni-mushroom-weathering-formation-of-st-ioannis\\\/\\\">Tafoni \\u2013 Mushroom weathering formation of St. Ioannis<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/tafoni-mushroom-weathering-formation-of-st-ioannis\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Fascinating erosion formations can be found in the volcanic rocks near the church of St. Ioannis in the area of Saint Ioannis Kaspakas on the west coast of Lemnos. The enormous voids seen in the rocky coastline of volcanic lavas are known as \\\"tafoni,\\\" and they are the products of erosion. The term \\\"tafoni\\\" means [&hellip;]<\\\/p>\\n\",\"address\":\"W3FC+57 \\u0386\\u03b3\\u03b9\\u03bf\\u03c2 \\u0399\\u03c9\\u03ac\\u03bd\\u03bd\\u03b7\\u03c2, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.922882750531045\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.070632537364975\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/tafoni-mushroom-weathering-formation-of-st-ioannis\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Fascinating erosion formations can be found in the volcanic rocks near the church of St. Ioannis in the area of Saint Ioannis Kaspakas on the west coast of Lemnos. The enormous voids seen in the rocky coastline of volcanic lavas are known as \\\"tafoni,\\\" and they are the products of erosion. The term \\\"tafoni\\\" means [&hellip;]<\\\/p>\\n\",\"post_content\":\"<div class=\\\"sections__field-body\\\">\\r\\n<div class=\\\"sections__field-body\\\">\\r\\n\\r\\nFascinating erosion formations can be found in the volcanic rocks near the church of St. Ioannis in the area of Saint Ioannis Kaspakas on the west coast of Lemnos.\\r\\n\\r\\nThe enormous voids seen in the rocky coastline of volcanic lavas are known as \\\"tafoni,\\\" and they are the products of erosion. The term \\\"tafoni\\\" means \\\"window\\\" in the Corsican dialect. The erosive force of water, wind, and sea spray loosens the crystals of the minerals in the volcanic rocks and causes the hollowing out of these \\u201ctafoni\\u201d.\\r\\n\\r\\n<\\\/div>\\r\\n<\\\/div>\",\"post_title\":\"Tafoni \\u2013 Mushroom weathering formation of St. Ioannis\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/tafoni-mushroom-weathering-formation-of-st-ioannis\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Tafoni \\u2013 Mushroom weathering formation of St. Ioannis\\\" width=\\\"300\\\" height=\\\"226\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/6-\\u03a4\\u03b1\\u03c6\\u03cc\\u03bd\\u03b9-\\u0391\\u03b3\\u03af\\u03bf\\u03c5-\\u0399\\u03c9\\u03ac\\u03bd\\u03bd\\u03b7-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.92288\",\"%wpcf-longtitude%\":\"25.07063\",\"%wpcf-location%\":\"\\u0386\\u03b3\\u03b9\\u03bf\\u03c2 \\u0399\\u03c9\\u03ac\\u03bd\\u03bd\\u03b7\\u03c2, \\u039a\\u03ac\\u03c3\\u03c0\\u03b1\\u03ba\\u03b1\\u03c2\",\"%_wpgmp_metabox_latitude%\":\"39.922882750531045\",\"%_wpgmp_metabox_longitude%\":\"25.070632537364975\",\"%_wpgmp_location_address%\":\"W3FC+57 \\u0386\\u03b3\\u03b9\\u03bf\\u03c2 \\u0399\\u03c9\\u03ac\\u03bd\\u03bd\\u03b7\\u03c2, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"%_wpgmp_location_city%\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"3\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/geoforms.png\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2749\",\"%_edit_lock%\":\"1657782189:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%84%ce%b1%cf%86%cf%8c%ce%bd%ce%b9-%ce%b1%ce%b3%ce%af%ce%bf%cf%85-%ce%b9%cf%89%ce%ac%ce%bd%ce%bd%ce%b7\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/6-\\u03a4\\u03b1\\u03c6\\u03cc\\u03bd\\u03b9-\\u0391\\u03b3\\u03af\\u03bf\\u03c5-\\u0399\\u03c9\\u03ac\\u03bd\\u03bd\\u03b7.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20989\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/6-\\u03a4\\u03b1\\u03c6\\u03cc\\u03bd\\u03b9-\\u0391\\u03b3\\u03af\\u03bf\\u03c5-\\u0399\\u03c9\\u03ac\\u03bd\\u03bd\\u03b7.jpg, 6-\\u03a4\\u03b1\\u03c6\\u03cc\\u03bd\\u03b9 \\u0391\\u03b3\\u03af\\u03bf\\u03c5 \\u0399\\u03c9\\u03ac\\u03bd\\u03bd\\u03b7, \",\"%_et_pb_truncate_post%\":\"<p>Fascinating erosion formations can be found in the volcanic rocks near the church of St. Ioannis in the area of Saint Ioannis Kaspakas on the west coast of Lemnos.<\\\/p>\\n<p>The enormous voids seen in the rocky coastline of volcanic lavas are known as &#8220;tafoni,&#8221; and they are the products of erosion. 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\\u2013 Erosion geoforms\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/geoforms_result-small.png\"},\"id\":3636,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/geoforms_result-small.png\",\"name\":\"\\u0393\\u03b5\\u03c9\\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2 \\u0391\\u03c0\\u03bf\\u03c3\\u03ac\\u03b8\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-\\u0394\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2\",\"id\":\"3\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Erosion Structures &#8211; Trigies Cape\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Erosion Structures &#8211; Trigies Cape\\\" width=\\\"300\\\" height=\\\"197\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/28-\\u039c\\u03b1\\u03bd\\u03b9\\u03c4\\u03b1\\u03c1\\u03bf\\u03b5\\u03b9\\u03b4\\u03b5\\u03af\\u03c2-\\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2-\\u03b1\\u03c0\\u03bf\\u03c3\\u03ac\\u03b8\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-\\u03b1\\u03ba\\u03c1\\u03c9\\u03c4\\u03b7\\u03c1\\u03af\\u03bf\\u03c5-\\u03a4\\u03c1\\u03b9\\u03b3\\u03b9\\u03ad\\u03c2-scaled-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/erosion-structures-trigies-cape\\\/\\\">Erosion Structures &#8211; Trigies Cape<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/erosion-structures-trigies-cape\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>In the sandstone cliffs of Trigies Cape, near the village of Atsiki in northern Lemnos, there are remarkable honeycomb and mushroom weathering formations. The mushroom weathering forms are caused by the action of the wind and sea spray. The wind creates the disintegration phenomena, which erodes the less cohesive clay layers as opposed to the [&hellip;]<\\\/p>\\n\",\"address\":\"X7QF+J6 \\u0391\\u03c4\\u03c3\\u03b9\\u03ba\\u03ae, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.98922234043897\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.272866817474373\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/erosion-structures-trigies-cape\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>In the sandstone cliffs of Trigies Cape, near the village of Atsiki in northern Lemnos, there are remarkable honeycomb and mushroom weathering formations. The mushroom weathering forms are caused by the action of the wind and sea spray. The wind creates the disintegration phenomena, which erodes the less cohesive clay layers as opposed to the [&hellip;]<\\\/p>\\n\",\"post_content\":\"In the sandstone cliffs of Trigies Cape, near the village of Atsiki in northern Lemnos, there are remarkable honeycomb and mushroom weathering formations.\\r\\n\\r\\nThe mushroom weathering forms are caused by the action of the wind and sea spray. The wind creates the disintegration phenomena, which erodes the less cohesive clay layers as opposed to the more cohesive sandy layers.\\r\\n\\r\\nTypical honeycomb weathering structures have also been discovered in coastal formations.\",\"post_title\":\"Erosion Structures &#8211; Trigies Cape\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/erosion-structures-trigies-cape\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Erosion Structures &#8211; Trigies Cape\\\" width=\\\"300\\\" height=\\\"197\\\" 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\\u2013 Erosion geoforms\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/geoforms_result-small.png\"},\"id\":3638,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/geoforms_result-small.png\",\"name\":\"\\u0393\\u03b5\\u03c9\\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2 \\u0391\\u03c0\\u03bf\\u03c3\\u03ac\\u03b8\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-\\u0394\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2\",\"id\":\"3\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Faraklo Spheroidal Weathering\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Faraklo Spheroidal Weathering\\\" width=\\\"300\\\" height=\\\"224\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/IMG_3610-scaled-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/faraklo-spheroidal-weathering\\\/\\\">Faraklo Spheroidal Weathering<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/faraklo-spheroidal-weathering\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Impressive patterns of spheroidal erosion emerge in sandstone layers in Faraklo, north of the village of Atsiki along the northern coasts of Lemnos. Upper Eocene-Lower Oligocene sedimentary layers formed in an underwater channel 27-33 million years ago cover the region. The chemical weathering of the layered sandstones produces geoforms of exceptional natural beauty, capturing the [&hellip;]<\\\/p>\\n\",\"address\":\"X6VR+HG \\u0391\\u03c4\\u03c3\\u03b9\\u03ba\\u03ae, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.994002907379\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.241255839347836\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/faraklo-spheroidal-weathering\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Impressive patterns of spheroidal erosion emerge in sandstone layers in Faraklo, north of the village of Atsiki along the northern coasts of Lemnos. Upper Eocene-Lower Oligocene sedimentary layers formed in an underwater channel 27-33 million years ago cover the region. The chemical weathering of the layered sandstones produces geoforms of exceptional natural beauty, capturing the [&hellip;]<\\\/p>\\n\",\"post_content\":\"Impressive patterns of spheroidal erosion emerge in sandstone layers in Faraklo, north of the village of Atsiki along the northern coasts of Lemnos.\\r\\n\\r\\nUpper Eocene-Lower Oligocene sedimentary layers formed in an underwater channel 27-33 million years ago cover the region.\\r\\n\\r\\nThe chemical weathering of the layered sandstones produces geoforms of exceptional natural beauty, capturing the curiosity of tourists who appreciate nature's uncommon masterpieces.\\r\\n\\r\\nThe spheroidal landforms reveal as large red spheres within the light-colored weathered sandstone. Networks of fractures are weathered into the sandstone rocks over time, allowing water to seep through and deepen these cracks. The endless action of the sea waves and salt from the sea spray compound this process started by the weathering, and the result is the creation of more of these beautiful spheroidal geoforms surrounded by sandstone rock.\",\"post_title\":\"Faraklo Spheroidal Weathering\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/faraklo-spheroidal-weathering\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Faraklo Spheroidal Weathering\\\" width=\\\"300\\\" height=\\\"224\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/IMG_3610-scaled-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" 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\\u2013 Erosion geoforms\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/geoforms_result-small.png\"},\"id\":3640,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/geoforms_result-small.png\",\"name\":\"\\u0393\\u03b5\\u03c9\\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2 \\u0391\\u03c0\\u03bf\\u03c3\\u03ac\\u03b8\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-\\u0394\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2\",\"id\":\"3\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Kakaviotissa Cave\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Kakaviotissa Cave\\\" width=\\\"300\\\" height=\\\"209\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/16-\\u03a3\\u03c0\\u03ae\\u03bb\\u03b1\\u03b9\\u03bf-\\u039a\\u03b1\\u03ba\\u03b1\\u03b2\\u03b9\\u03ce\\u03c4\\u03b9\\u03c3\\u03c3\\u03b1\\u03c22-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kakaviotissa-cave\\\/\\\">Kakaviotissa Cave<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kakaviotissa-cave\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 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To reach the cave, visitors must first ascend the volcanic hill of Kakavos made of andesitic lava. At the summit of the hill, weathering formations are visible. These are \\\"tafoni,\\\" which are cavities formed by the erosion of [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.865\",\"lng\":\"25.107\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kakaviotissa-cave\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The cave of Kakaviotissa is located in the area of Kakavos, northeast of the village of Thanos. To reach the cave, visitors must first ascend the volcanic hill of Kakavos made of andesitic lava. At the summit of the hill, weathering formations are visible. These are \\\"tafoni,\\\" which are cavities formed by the erosion of [&hellip;]<\\\/p>\\n\",\"post_content\":\"<div class=\\\"sections__field-body\\\">\\r\\n\\r\\nThe cave of Kakaviotissa is located in the area of Kakavos, northeast of the village of Thanos. To reach the cave, visitors must first ascend the volcanic hill of Kakavos made of andesitic lava. At the summit of the hill, weathering formations are visible. These are \\\"tafoni,\\\" which are cavities formed by the erosion of volcanic rocks. Today, the church of Panagia Kakaviotissa is constructed in the largest of these cavities.\\r\\n\\r\\nThe term \\\"tafoni\\\" is derived from the Corsican word for \\\"window\\\" and is used around the globe to characterize these distinctive honeycomb weathering patterns seen in granular igneous and sedimentary rocks. Their appearance is determined by the selective or differential erosion of the rock surface. 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\\u2013 Erosion geoforms\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/geoforms_result-small.png\"},\"id\":3643,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/geoforms_result-small.png\",\"name\":\"\\u0393\\u03b5\\u03c9\\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2 \\u0391\\u03c0\\u03bf\\u03c3\\u03ac\\u03b8\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-\\u0394\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2\",\"id\":\"3\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Erosion formations of St. Ermolaos\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Erosion formations of St. Ermolaos\\\" width=\\\"300\\\" height=\\\"217\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/27-\\u039c\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2-\\u03b4\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-\\u0391\\u03b3\\u03af\\u03bf\\u03c5-\\u0395\\u03c1\\u03bc\\u03bf\\u03bb\\u03ac\\u03bf\\u03c5-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/erosion-formations-of-st-ermolaos\\\/\\\">Erosion formations of St. Ermolaos<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/erosion-formations-of-st-ermolaos\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Remarkable basin-like formations of erosion in the sandstone layers can be found in the region of St. Ermolaos, a few kilometers north of the village of Varos on the northern coasts of Lemnos. The region is covered with Upper Eocene-Lower Oligocene sedimentary layers deposited in underwater channels 27-33 million years ago. Formed by the erosion [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.968269\",\"lng\":\"25.266536\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/erosion-formations-of-st-ermolaos\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Remarkable basin-like formations of erosion in the sandstone layers can be found in the region of St. Ermolaos, a few kilometers north of the village of Varos on the northern coasts of Lemnos. The region is covered with Upper Eocene-Lower Oligocene sedimentary layers deposited in underwater channels 27-33 million years ago. Formed by the erosion [&hellip;]<\\\/p>\\n\",\"post_content\":\"<div class=\\\"sections__field-body\\\">\\r\\n\\r\\nRemarkable basin-like formations of erosion in the sandstone layers can be found in the region of St. Ermolaos, a few kilometers north of the village of Varos on the northern coasts of Lemnos.\\r\\n\\r\\nThe region is covered with Upper Eocene-Lower Oligocene sedimentary layers deposited in underwater channels 27-33 million years ago.\\r\\n\\r\\nFormed by the erosion of sandstone rocks, the basin-like features fascinate visitors with their stunning forms.\\r\\n\\r\\nThe differential erosion is caused mostly by the different composition of the rock, which means sea water and salt from the sea spray and can break through its weaker surfaces and begin the process of erosion.\\r\\n\\r\\n<\\\/div>\",\"post_title\":\"Erosion formations of St. 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21180, 21181, 21182, 21183, 21184, 21185, 21186\",\"%wpcf-code%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/IMG_4240-scaled.jpg, IMG_4240, \",\"%_et_pb_truncate_post%\":\"<p>Remarkable basin-like formations of erosion in the sandstone layers can be found in the region of St. Ermolaos, a few kilometers north of the village of Varos on the northern coasts of Lemnos.<\\\/p>\\n<p>The region is covered with Upper Eocene-Lower Oligocene sedimentary layers deposited in underwater channels 27-33 million years ago.<\\\/p>\\n<p>Formed by the erosion of sandstone rocks, the basin-like features fascinate visitors with their stunning forms.<\\\/p>\\n<p>The differential erosion is caused mostly by the different composition of the rock, which means sea water and salt from the sea spray and can break through its weaker surfaces and begin the process of 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\\u2013 Erosion geoforms\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/geoforms_result-small.png\"},\"id\":3645,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/geoforms_result-small.png\",\"name\":\"\\u0393\\u03b5\\u03c9\\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2 \\u0391\\u03c0\\u03bf\\u03c3\\u03ac\\u03b8\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-\\u0394\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2\",\"id\":\"3\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Tafoni of Myrina\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Tafoni of Myrina\\\" width=\\\"300\\\" height=\\\"193\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/37-tafoni-murinas-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/tafoni-of-myrina\\\/\\\">Tafoni of Myrina<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/tafoni-of-myrina\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Impressive formations of honeycomb weathering appears on the volcanic rocks of the hill on which the medieval castle of Myrina is constructed. The volcanic rocks comprise a large volcanic dome that formed 19 million years ago as a result of andesitic lava penetrating pre-existing rocks. The erosion of the surface rocks revealed Myrina's volcanic dome. [&hellip;]<\\\/p>\\n\",\"address\":\"V3F4+XV \\u039c\\u03cd\\u03c1\\u03b9\\u03bd\\u03b1, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.87493059377014\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.057288190216056\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/tafoni-of-myrina\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Impressive formations of honeycomb weathering appears on the volcanic rocks of the hill on which the medieval castle of Myrina is constructed. The volcanic rocks comprise a large volcanic dome that formed 19 million years ago as a result of andesitic lava penetrating pre-existing rocks. The erosion of the surface rocks revealed Myrina's volcanic dome. [&hellip;]<\\\/p>\\n\",\"post_content\":\"Impressive formations of honeycomb weathering appears on the volcanic rocks of the hill on which the medieval castle of Myrina is constructed.\\r\\n\\r\\nThe volcanic rocks comprise a large volcanic dome that formed 19 million years ago as a result of andesitic lava penetrating pre-existing rocks. The erosion of the surface rocks revealed Myrina's volcanic dome. On the surface of these volcanic rocks, modern erosion processes have created large or small erosion caverns in the rocks such as these \\\"tafoni,\\\" or honeycomb structures.\\r\\n\\r\\n\\\"Tafoni\\\" are the formations which created by the differential erosion of the rock surface, caused primarily by the features of the rock (granular composition, strength, lithology), but also by external factors.\\r\\n\\r\\nThe term \\\"tafoni\\\" is derived from the Corsican word for \\\"window\\\" and is used around the world to characterize these distinctive structures of erosion found mostly in igneous rocks.\",\"post_title\":\"Tafoni of Myrina\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/tafoni-of-myrina\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Tafoni of Myrina\\\" width=\\\"300\\\" height=\\\"193\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/37-tafoni-murinas-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.87493\",\"%wpcf-longtitude%\":\"25.05728\",\"%wpcf-location%\":\"\\u039c\\u03cd\\u03c1\\u03b9\\u03bd\\u03b1\",\"%_wpgmp_metabox_latitude%\":\"39.87493059377014\",\"%_wpgmp_metabox_longitude%\":\"25.057288190216056\",\"%_wpgmp_location_address%\":\"V3F4+XV \\u039c\\u03cd\\u03c1\\u03b9\\u03bd\\u03b1, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"%_wpgmp_location_city%\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"3\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/geoforms.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"3062\",\"%_edit_lock%\":\"1657786636:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%80%ce%b1%ce%bb%ce%b1%ce%b9%cf%8c%ce%ba%ce%b1%cf%83%cf%84%cf%81%ce%bf-%cf%80%ce%bb%ce%ac%ce%ba%ce%b1%cf%82\",\"%wpcf-code%\":\"\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/37-tafoni-murinas.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"21227\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/37-tafoni-murinas.jpg, 37-tafoni murinas, \",\"%_et_pb_truncate_post%\":\"<p>Impressive formations of honeycomb weathering appears on the volcanic rocks of the hill on which the medieval castle of Myrina is constructed.<\\\/p>\\n<p>The volcanic rocks comprise a large volcanic dome that formed 19 million years ago as a result of andesitic lava penetrating pre-existing rocks. 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On the surface of these volcanic rocks, modern erosion processes have created large or small erosion caverns in the rocks such as these &#8220;tafoni,&#8221; or honeycomb structures.<\\\/p>\\n<p>&#8220;Tafoni&#8221; are the formations which created by the differential erosion of the rock surface, caused primarily by the features of the rock (granular composition, strength, lithology), but also by external factors.<\\\/p>\\n<p>The term &#8220;tafoni&#8221; is derived from the Corsican word for &#8220;window&#8221; and is used around the world to characterize these distinctive structures of erosion found mostly in igneous rocks.<\\\/p>\\n\",\"%_et_pb_truncate_post_date%\":\"2023-09-09 11:34:45\",\"%_et_dynamic_cached_shortcodes%\":\"et_pb_section, et_pb_row, et_pb_column, et_pb_text, et_pb_sidebar, et_pb_divider, et_pb_code, et_pb_image, et_pb_social_media_follow, 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\\u2013 Erosion geoforms\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/geoforms_result-small.png\"},\"id\":3648,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/geoforms_result-small.png\",\"name\":\"\\u0393\\u03b5\\u03c9\\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2 \\u0391\\u03c0\\u03bf\\u03c3\\u03ac\\u03b8\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-\\u0394\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2\",\"id\":\"3\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Erosion Formations of St. Efthymia\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Erosion Formations of St. Efthymia\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/IMG_7501-scaled-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/erosion-formations-of-st-efthymia\\\/\\\">Erosion Formations of St. Efthymia<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/erosion-formations-of-st-efthymia\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Northeast of the village of Propouli, in the coastal region near the church of Agia Efthymia, impressive forms of erosion in the sandstone rocks are of the Upper Iocene - Lower Oligocene age. The region is covered with sedimentary formations made up of sandstones and siltstones that were formed in underwater channels between 27 and [&hellip;]<\\\/p>\\n\",\"address\":\"X7P8+97 \\u0391\\u03c4\\u03c3\\u03b9\\u03ba\\u03ae, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.98589381653119\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.26566053833008\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/erosion-formations-of-st-efthymia\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Northeast of the village of Propouli, in the coastal region near the church of Agia Efthymia, impressive forms of erosion in the sandstone rocks are of the Upper Iocene - Lower Oligocene age. The region is covered with sedimentary formations made up of sandstones and siltstones that were formed in underwater channels between 27 and [&hellip;]<\\\/p>\\n\",\"post_content\":\"Northeast of the village of Propouli, in the coastal region near the church of Agia Efthymia, impressive forms of erosion in the sandstone rocks are of the Upper Iocene - Lower Oligocene age.\\r\\n\\r\\nThe region is covered with sedimentary formations made up of sandstones and siltstones that were formed in underwater channels between 27 and 33 million years ago.\\r\\n\\r\\nThe honeycomb and basin-like formations seen in the sandstone layers across the coastal zone are the result of differential erosion caused by the action of water, waves, and the crystallization of salts deposited by sea spray are the primary causes of differential erosion.\",\"post_title\":\"Erosion Formations of St. 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