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_builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding_tablet=&#8221;20px|50px|20px|50px|true|true&#8221; custom_padding_phone=&#8221;10px|20px|10px|20px|true|true&#8221; custom_padding_last_edited=&#8221;off|desktop&#8221; global_colors_info=&#8221;{}&#8221; padding_phone=&#8221;10px|20px|10px|20px|true|true&#8221; padding_tablet=&#8221;20px|50px|20px|50px|true|true&#8221; padding_last_edited=&#8221;off|desktop&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_text _builder_version=&#8221;4.11.4&#8243; text_font=&#8221;||||||||&#8221; text_font_size=&#8221;16px&#8221; text_line_height=&#8221;2em&#8221; text_orientation=&#8221;justified&#8221; custom_padding=&#8221;|16px|0px|17px||&#8221; hover_enabled=&#8221;0&#8243; text_font_size_tablet=&#8221;14px&#8221; text_font_size_phone=&#8221;&#8221; text_font_size_last_edited=&#8221;on|tablet&#8221; global_colors_info=&#8221;{}&#8221; sticky_enabled=&#8221;0&#8243;]<\/p>\n<p><strong>Geosites of Lemnos<br \/><\/strong><\/p>\n<p>Lemnos is located in the northeastern Aegean, between mount Athos and the island of Lesvos. \u00a0It is a volcanic island; one can locate many volcanoes, aging approximately 23 million years, rising proudly from the soil. Sedimentary formations aging about 33 million years dominate the central and eastern regions.<\/p>\n<p>The island is filled with geosites of captivating beauty. Fossil sites, volcanic structures, tectonic geosites, erosion and deposit geoforms, coastal geosites, water systems and man-made sites formulate the types of geosites one can explore on the island.<\/p>\n<p>With the term \u201cgeosite,\u201d we characterize the elements which we aim to protect through an environmental law (\u039d. 1650\/1986, \u039d. 3937\/2011) and which function as important signs and indications of the history of the earth.<\/p>\n<p>Lemnos island\u2019s geosites present themselves yet remain hidden. They await exploration as most people are not aware of them. 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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. 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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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src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/23-\\u03b2\\u03b1\\u03c1\\u03bf\\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\\\/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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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. 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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.<\\\/p>\\n<p>First mentioned by Herodotus, the healing abilities of the &#8220;Limnian Earth&#8221; are mythologically connected with Hephaestus whose wounds were healed by them following his expulsion from Olympus. The story of the Pergamon doctor Galinos who visited Lemnos in 167 BC and purchased 20,000 &#8220;Limnian Earth&#8221; pills, is also\\u00a0fascinating.<\\\/p>\\n<p>During the Byzantine and Ottoman periods, the extraction and trade of important materials was strictly regulated, and this product was sold in sealed disk like shapes, thus the name &#8220;Terra Siggilata&#8221; (sealed earth). 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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\":\"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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global_colors_info=&#8221;{}&#8221;]<\/p>\n<p><span style=\"font-size: large;\"><strong>Geosites<\/strong><\/span><\/p>\n<ul>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/geosites\/volcanos\/\"><span style=\"color: #ffffff;\">Volcanic Geosites<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/geosites\/apolithomata\/\"><span style=\"color: #ffffff;\">Fossils<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/geosites\/tektonikoi\/\"><span style=\"color: #ffffff;\">Tectonic Geosites<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/geosites\/water\/\"><span style=\"color: #ffffff;\">Hydrographic Systems<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/geosites\/%cf%80%ce%b1%cf%81%ce%ac%ce%ba%cf%84%ce%b9%ce%b5%cf%82-%ce%b3%ce%b5%cf%89%ce%bc%ce%bf%cf%81%cf%86%ce%ad%cf%82\/\"><span style=\"color: #ffffff;\">Coastal Geosites<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/geosites\/geomorfology\/\"><span style=\"color: #ffffff;\">Weathering-Erosion Geosites<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/geosites\/geoapotheseis\/\"><span style=\"color: #ffffff;\">Deposit Geoforms<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/geosites\/anthropogeneis\/\"><span style=\"color: #ffffff;\">Man-made Sites<\/span><\/a><\/li>\n<\/ul>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8221;1_4&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; global_colors_info=&#8221;{}&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_text ul_type=&#8221;square&#8221; _builder_version=&#8221;4.11.4&#8243; text_font=&#8221;||||||||&#8221; text_text_color=&#8221;#FFFFFF&#8221; link_font=&#8221;||||||||&#8221; link_text_color=&#8221;#ffba5a&#8221; ul_font=&#8221;||||||||&#8221; quote_font=&#8221;||||||||&#8221; custom_margin=&#8221;10px|||||&#8221; locked=&#8221;off&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<p><span style=\"font-size: large;\"><strong>Culture<\/strong><\/span><\/p>\n<ul>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/culture\/ancient_sites\/\"><span style=\"color: #ffffff;\">Archaeological Sites<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/culture\/churches\/\"><span style=\"color: #ffffff;\">Religious Monuments<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/culture\/monuments\/\"><span style=\"color: #ffffff;\">Modern Monuments<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/culture\/villages\/\"><span style=\"color: #ffffff;\">Lemnos Settlements<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/culture\/museums\/\"><span style=\"color: #ffffff;\">Museums<\/span><\/a><\/li>\n<\/ul>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8221;1_4&#8243; 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follow_button=&#8221;off&#8221; url_new_window=&#8221;on&#8221;]twitter[\/et_pb_social_media_follow_network][et_pb_social_media_follow_network social_network=&#8221;linkedin&#8221; _builder_version=&#8221;3.18.2&#8243; custom_padding=&#8221;10px|10px|10px|10px|true|true&#8221; global_colors_info=&#8221;{}&#8221; follow_button=&#8221;off&#8221; url_new_window=&#8221;on&#8221;]linkedin[\/et_pb_social_media_follow_network][\/et_pb_social_media_follow][et_pb_image src=&#8221;\/wp-content\/uploads\/2021\/07\/Sticker-website_EDET_GR_HighRes-1-scaled.jpg&#8221; title_text=&#8221;Sticker-website_EDET_GR_HighRes&#8221; align=&#8221;center&#8221; _builder_version=&#8221;4.11.3&#8243; _module_preset=&#8221;default&#8221; border_radii=&#8221;on|5px|5px|5px|5px&#8221; global_colors_info=&#8221;{}&#8221;][\/et_pb_image][et_pb_text _builder_version=&#8221;4.11.4&#8243; _module_preset=&#8221;default&#8221; text_orientation=&#8221;center&#8221; background_layout=&#8221;dark&#8221; custom_margin=&#8221;||5%||false|false&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<p>This website was implemented with the co-financing of Greece and the European Union<\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"<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 &#8211; Lower Oligocene age. 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