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custom_padding=&#8221;30px|20px|30px|20px|true|true&#8221; link_option_url=&#8221;@ET-DC@eyJkeW5hbWljIjp0cnVlLCJjb250ZW50IjoicG9zdF9saW5rX3VybF9wYWdlIiwic2V0dGluZ3MiOnsicG9zdF9pZCI6IjE3MTcifX0=@&#8221; locked=&#8221;off&#8221; global_colors_info=&#8221;{}&#8221; custom_margin__hover_enabled=&#8221;on|hover&#8221; custom_padding__hover_enabled=&#8221;on&#8221; custom_padding__hover=&#8221;30px||30px||true|true&#8221; custom_margin__hover=&#8221;0px||&#8221; box_shadow_style__hover=&#8221;none&#8221; box_shadow_style__hover_enabled=&#8221;none&#8221; box_shadow_color__hover=&#8221;rgba(0,0,0,0.3)&#8221; box_shadow_color__hover_enabled=&#8221;rgba(0,0,0,0.3)&#8221; border_radii__hover=&#8221;on||||&#8221; border_radii__hover_enabled=&#8221;on|hover&#8221;]<\/p>\n<p>3d models<\/p>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8221;1_5&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; global_colors_info=&#8221;{}&#8221; 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custom_margin__hover=&#8221;0px||&#8221; box_shadow_style__hover=&#8221;none&#8221; box_shadow_style__hover_enabled=&#8221;none&#8221; box_shadow_color__hover=&#8221;rgba(0,0,0,0.3)&#8221; box_shadow_color__hover_enabled=&#8221;rgba(0,0,0,0.3)&#8221; border_radii__hover=&#8221;on||||&#8221; border_radii__hover_enabled=&#8221;on|hover&#8221;]<\/p>\n<p>Video<\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=&#8221;1&#8243; admin_label=&#8221;Blog&#8221; _builder_version=&#8221;3.22&#8243; custom_padding=&#8221;||4px|||&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_row custom_padding_last_edited=&#8221;on|phone&#8221; padding_top_bottom_link_1=&#8221;true&#8221; padding_left_right_link_1=&#8221;true&#8221; _builder_version=&#8221;4.11.4&#8243; max_width=&#8221;1127px&#8221; custom_margin=&#8221;3px|auto||auto||&#8221; custom_padding=&#8221;14px|10px|14px|10px|true|true&#8221; custom_padding_tablet=&#8221;40px|40px|40px|40px|true|true&#8221; custom_padding_phone=&#8221;20px|20px|20px|20px|true|true&#8221; animation_style=&#8221;flip&#8221; animation_direction=&#8221;left&#8221; animation_intensity_flip=&#8221;10%&#8221; box_shadow_style=&#8221;preset3&#8243; box_shadow_vertical=&#8221;32px&#8221; box_shadow_blur=&#8221;200px&#8221; box_shadow_spread=&#8221;-16px&#8221; box_shadow_color=&#8221;rgba(85,103,127,0.3)&#8221; use_custom_width=&#8221;on&#8221; custom_width_px=&#8221;900px&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;4_4&#8243; _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||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>Coastal Geosites<br \/><\/strong><\/p>\n<p>Stunning coastal geosites along the coast of Lemnos are the work of the endless movement of the sea waves and the driving wind upon the seaside rocks.<\/p>\n<p>Columnar geoforms, arches, tafoni, underwater caves, tombolos, beachrocks, and erosion structures of coastal geological formations are some of the types of coastal geoforms found on Lemnos, with places of note being Cape Mourtzeflos, the Filokrotis cave, the Louri beach etc..<\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;||0px|||&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;4_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 _builder_version=&#8221;4.11.4&#8243; header_font=&#8221;||||||||&#8221; header_2_font=&#8221;Noto Serif||||||||&#8221; header_2_font_size=&#8221;40px&#8221; header_2_line_height=&#8221;1.4em&#8221; custom_margin=&#8221;||5px|||&#8221; header_2_font_size_tablet=&#8221;30px&#8221; header_2_font_size_phone=&#8221;24px&#8221; header_2_font_size_last_edited=&#8221;on|phone&#8221; locked=&#8221;off&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<h3>Sites of interest<\/h3>\n<p>[\/et_pb_text][et_pb_divider color=&#8221;#a5bab1&#8243; divider_weight=&#8221;3px&#8221; _builder_version=&#8221;4.9.7&#8243; 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custom_width_px__hover_enabled=&#8221;1080px&#8221; custom_width_percent__hover=&#8221;80%&#8221; custom_width_percent__hover_enabled=&#8221;80%&#8221; collapsed=&#8221;off&#8221; global_colors_info=&#8221;{}&#8221; gutter_width__hover=&#8221;3&#8243; gutter_width__hover_enabled=&#8221;3&#8243; parallax_1__hover=&#8221;off&#8221; parallax_1__hover_enabled=&#8221;off&#8221; parallax_2__hover=&#8221;off&#8221; parallax_2__hover_enabled=&#8221;off&#8221; parallax_3__hover=&#8221;off&#8221; parallax_3__hover_enabled=&#8221;off&#8221; parallax_method_1__hover=&#8221;on&#8221; parallax_method_1__hover_enabled=&#8221;on&#8221; parallax_method_2__hover=&#8221;on&#8221; parallax_method_2__hover_enabled=&#8221;on&#8221; parallax_method_3__hover=&#8221;on&#8221; parallax_method_3__hover_enabled=&#8221;on&#8221; use_background_color_gradient__hover=&#8221;off&#8221; use_background_color_gradient__hover_enabled=&#8221;off&#8221; background_color_gradient_start__hover=&#8221;#2b87da&#8221; background_color_gradient_start__hover_enabled=&#8221;#2b87da&#8221; background_color_gradient_end__hover=&#8221;#29c4a9&#8243; background_color_gradient_end__hover_enabled=&#8221;#29c4a9&#8243; background_color_gradient_type__hover=&#8221;linear&#8221; background_color_gradient_type__hover_enabled=&#8221;linear&#8221; background_color_gradient_direction__hover=&#8221;180deg&#8221; background_color_gradient_direction__hover_enabled=&#8221;180deg&#8221; background_color_gradient_direction_radial__hover=&#8221;center&#8221; background_color_gradient_direction_radial__hover_enabled=&#8221;center&#8221; background_color_gradient_start_position__hover=&#8221;0%&#8221; background_color_gradient_start_position__hover_enabled=&#8221;0%&#8221; background_color_gradient_end_position__hover=&#8221;100%&#8221; background_color_gradient_end_position__hover_enabled=&#8221;100%&#8221; background_color_gradient_overlays_image__hover=&#8221;off&#8221; 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make_fullwidth__hover_enabled=&#8221;off&#8221; use_custom_width__hover=&#8221;off&#8221; use_custom_width__hover_enabled=&#8221;off&#8221; width_unit__hover=&#8221;on&#8221; width_unit__hover_enabled=&#8221;on&#8221; make_equal__hover=&#8221;off&#8221; make_equal__hover_enabled=&#8221;off&#8221; use_custom_gutter__hover=&#8221;off&#8221; use_custom_gutter__hover_enabled=&#8221;off&#8221; border_radii__hover=&#8221;on||||&#8221; border_radii__hover_enabled=&#8221;on||||&#8221; box_shadow_style__hover=&#8221;none&#8221; box_shadow_style__hover_enabled=&#8221;none&#8221; box_shadow_color__hover=&#8221;rgba(0,0,0,0.3)&#8221; box_shadow_color__hover_enabled=&#8221;rgba(0,0,0,0.3)&#8221; max_width__hover=&#8221;100%&#8221; max_width__hover_enabled=&#8221;100%&#8221; filter_hue_rotate__hover=&#8221;0deg&#8221; filter_hue_rotate__hover_enabled=&#8221;0deg&#8221; filter_saturate__hover=&#8221;100%&#8221; filter_saturate__hover_enabled=&#8221;100%&#8221; 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animation_duration__hover_enabled=&#8221;1000ms&#8221; animation_delay__hover=&#8221;0ms&#8221; animation_delay__hover_enabled=&#8221;0ms&#8221; animation_intensity_slide__hover=&#8221;50%&#8221; animation_intensity_slide__hover_enabled=&#8221;50%&#8221; animation_intensity_zoom__hover=&#8221;50%&#8221; animation_intensity_zoom__hover_enabled=&#8221;50%&#8221; animation_intensity_flip__hover=&#8221;50%&#8221; animation_intensity_flip__hover_enabled=&#8221;50%&#8221; animation_intensity_fold__hover=&#8221;50%&#8221; animation_intensity_fold__hover_enabled=&#8221;50%&#8221; animation_intensity_roll__hover=&#8221;50%&#8221; animation_intensity_roll__hover_enabled=&#8221;50%&#8221; animation_starting_opacity__hover=&#8221;0%&#8221; animation_starting_opacity__hover_enabled=&#8221;0%&#8221; animation_speed_curve__hover=&#8221;ease-in-out&#8221; animation_speed_curve__hover_enabled=&#8221;ease-in-out&#8221; hover_transition_duration__hover=&#8221;300ms&#8221; hover_transition_duration__hover_enabled=&#8221;300ms&#8221; hover_transition_delay__hover=&#8221;0ms&#8221; hover_transition_delay__hover_enabled=&#8221;0ms&#8221; hover_transition_speed_curve__hover=&#8221;ease&#8221; hover_transition_speed_curve__hover_enabled=&#8221;ease&#8221;][et_pb_row column_structure=&#8221;1_4,1_2,1_4&#8243; _builder_version=&#8221;4.9.7&#8243; _module_preset=&#8221;default&#8221; custom_padding=&#8221;||0px|||&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;1_4&#8243; _builder_version=&#8221;4.9.7&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_divider color=&#8221;#FFFFFF&#8221; divider_weight=&#8221;1px&#8221; _builder_version=&#8221;4.9.7&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][\/et_pb_divider][\/et_pb_column][et_pb_column type=&#8221;1_2&#8243; _builder_version=&#8221;4.9.7&#8243; _module_preset=&#8221;default&#8221; 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In many cases, the magma either reached the surface as thick lava or, after cooling at a shallow depth below the surface, was revealed by the erosion of the overlying geologic material, resulting in the formation of these distinctive volcanic structures in both cases.\\r\\n\\r\\nThe morphology of the coast and the separation of the islet from its adjoining land are the result of the movement of the NE-SW large Mourtzeflos strike-slip fault.\\r\\n\\r\\nTombolo is a coastal deposition formation composed primarily of sands and rounded pebbles (cobbles). 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The volcanic formation called the volcanic dome of Mourtzeflos appears as an islet composed of volcanic rocks of tracheandesitic composition, but it is joined to the mainland by a small sandy strip, forming the tombolo\\u2019s unique geomorphological structure.<\\\/p>\\n<p>Approximately 20-21 million years old, the volcanic structure\\u2019s formation is linked to a series of volcanic structures that were created on Western Lemnos during that period. These distinctive volcanic domes were formed by ascending viscous magma with a high gas content that penetrated the pre-existing sedimentary rocks, folding and uplifting them. In many cases, the magma either reached the surface as thick lava or, after cooling at a shallow depth below the surface, was revealed by the erosion of the overlying geologic material, resulting in the formation of these distinctive volcanic structures in both cases.<\\\/p>\\n<p>The morphology of the coast and the separation of the islet from its adjoining land are the result of the movement of the NE-SW large Mourtzeflos strike-slip fault.<\\\/p>\\n<p>Tombolo is a coastal deposition formation composed primarily of sands and rounded pebbles (cobbles). 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geosites\"},\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\"},\"id\":3582,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\",\"name\":\"\\u03a0\\u03b1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b9\\u03bf\\u03b9\",\"id\":\"14\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Filoktitis \\u2013 Kaveria Cave\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Filoktitis \\u2013 Kaveria Cave\\\" width=\\\"300\\\" height=\\\"155\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/32-\\u03a3\\u03c0\\u03b7\\u03bb\\u03b9\\u03ac-\\u03c4\\u03bf\\u03c5-\\u03a6\\u03b9\\u03bb\\u03bf\\u03ba\\u03c4\\u03ae\\u03c4\\u03b7-\\u039a\\u03b1\\u03b2\\u03b5\\u03af\\u03c1\\u03b9\\u03b13-scaled-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/filoktitis-kaveria-cave\\\/\\\">Filoktitis \\u2013 Kaveria Cave<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/filoktitis-kaveria-cave\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The cave of Filoktitis is located on the northeast coast of Lemnos near the archaeological complex of the Temple of Kaveria, one of Lemnos\\u2019 most important archaeological sites. A large concave has opened in the area\\u2019s sandstone cliffs going down towards the sea. Descending the steps carved into the sandstone rocks, the visitor reaches the [&hellip;]<\\\/p>\\n\",\"address\":\"X8JR+8R \\u039c\\u03bf\\u03cd\\u03b4\\u03c1\\u03bf\\u03c2, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.98077489984695\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.342096941406254\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/filoktitis-kaveria-cave\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The cave of Filoktitis is located on the northeast coast of Lemnos near the archaeological complex of the Temple of Kaveria, one of Lemnos\\u2019 most important archaeological sites. A large concave has opened in the area\\u2019s sandstone cliffs going down towards the sea. Descending the steps carved into the sandstone rocks, the visitor reaches the [&hellip;]<\\\/p>\\n\",\"post_content\":\"The cave of Filoktitis is located on the northeast coast of Lemnos near the archaeological complex of the Temple of Kaveria, one of Lemnos\\u2019 most important archaeological sites.\\r\\n\\r\\nA large concave has opened in the area\\u2019s sandstone cliffs going down towards the sea. Descending the steps carved into the sandstone rocks, the visitor reaches the opening. Inside this crevice is the underwater cave of Filoktitis, which can also be accessed by boat from the sea.\\r\\n\\r\\nThe cave is a type of coastal erosion in which sea waves erode rocks along geological discontinuities. The area\\u2019s sedimentary molassic rocks, in particular, cannot resist to the erosion processes, resulting in the creation of coastal caverns.\\r\\n\\r\\nAccording to mythology, Philoktitis lived in this cave for around 10 years after being bitten in the leg by a snake, which caused him to depart from the ship bound for Troy to fight in the Trojan War.\",\"post_title\":\"Filoktitis \\u2013 Kaveria Cave\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/filoktitis-kaveria-cave\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Filoktitis \\u2013 Kaveria Cave\\\" width=\\\"300\\\" height=\\\"155\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/32-\\u03a3\\u03c0\\u03b7\\u03bb\\u03b9\\u03ac-\\u03c4\\u03bf\\u03c5-\\u03a6\\u03b9\\u03bb\\u03bf\\u03ba\\u03c4\\u03ae\\u03c4\\u03b7-\\u039a\\u03b1\\u03b2\\u03b5\\u03af\\u03c1\\u03b9\\u03b13-scaled-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.980\",\"%wpcf-longtitude%\":\"25.341\",\"%_wpgmp_metabox_latitude%\":\"39.98077489984695\",\"%_wpgmp_metabox_longitude%\":\"25.342096941406254\",\"%_wpgmp_location_address%\":\"X8JR+8R \\u039c\\u03bf\\u03cd\\u03b4\\u03c1\\u03bf\\u03c2, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"%_wpgmp_location_city%\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"14\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi.png\",\"%wpcf-location%\":\"\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_wpml_location_migration_done%\":\"1\",\"%_wpml_word_count%\":\"{\\\"total\\\":171,\\\"to_translate\\\":{\\\"en\\\":171}}\",\"%_thumbnail_id%\":\"3037\",\"%_edit_lock%\":\"1655276461:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%83%cf%80%ce%b7%ce%bb%ce%b9%ce%ac-%cf%84%ce%bf%cf%85-%cf%86%ce%b9%ce%bb%ce%bf%ce%ba%cf%84%ce%ae%cf%84%ce%b7-%ce%ba%ce%b1%ce%b2%ce%b5%ce%af%cf%81%ce%b9%ce%b1\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/32-\\u03a3\\u03c0\\u03b7\\u03bb\\u03b9\\u03ac-\\u03c4\\u03bf\\u03c5-\\u03a6\\u03b9\\u03bb\\u03bf\\u03ba\\u03c4\\u03ae\\u03c4\\u03b7-\\u039a\\u03b1\\u03b2\\u03b5\\u03af\\u03c1\\u03b9\\u03b13.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20207, 20208, 20209\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/32-\\u03a3\\u03c0\\u03b7\\u03bb\\u03b9\\u03ac-\\u03c4\\u03bf\\u03c5-\\u03a6\\u03b9\\u03bb\\u03bf\\u03ba\\u03c4\\u03ae\\u03c4\\u03b7-\\u039a\\u03b1\\u03b2\\u03b5\\u03af\\u03c1\\u03b9\\u03b12-scaled.jpg, 32-\\u03a3\\u03c0\\u03b7\\u03bb\\u03b9\\u03ac \\u03c4\\u03bf\\u03c5 \\u03a6\\u03b9\\u03bb\\u03bf\\u03ba\\u03c4\\u03ae\\u03c4\\u03b7-\\u039a\\u03b1\\u03b2\\u03b5\\u03af\\u03c1\\u03b9\\u03b12, \",\"%_et_pb_truncate_post%\":\"<p>The cave of Filoktitis is located on the northeast coast of Lemnos near the archaeological complex of the Temple of Kaveria, one of Lemnos\\u2019 most important archaeological sites.<\\\/p>\\n<p>A large concave has opened in the area\\u2019s sandstone cliffs going down towards the sea. 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class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/fanarakis-sea-caves\\\/\\\">Fanaraki&#8217;s Sea Caves<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/fanarakis-sea-caves\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Southwest of Moudros, the Cape of Aspros Kavos features pyroclastic deposits with considerable hydrothermal alteration at the beaches of \\\"Mikro\\\" and \\\"Megalo Fanaraki\\\". Mineralogical, chemical, and structural changes occurred in the surrounding strata as a result of the impact of hot solutions of metal-rich water flowing in the pyroclastic materials. These alterations have resulted in [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.852\",\"lng\":\"25.237\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/fanarakis-sea-caves\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Southwest of Moudros, the Cape of Aspros Kavos features pyroclastic deposits with considerable hydrothermal alteration at the beaches of \\\"Mikro\\\" and \\\"Megalo Fanaraki\\\". Mineralogical, chemical, and structural changes occurred in the surrounding strata as a result of the impact of hot solutions of metal-rich water flowing in the pyroclastic materials. 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geosites\"},\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\"},\"id\":3584,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\",\"name\":\"\\u03a0\\u03b1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b9\\u03bf\\u03b9\",\"id\":\"14\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Prassa Limani Tombolo\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Prassa Limani Tombolo\\\" width=\\\"300\\\" height=\\\"210\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/4-\\u03a4\\u03cc\\u03bc\\u03c0\\u03bf\\u03bb\\u03bf-\\u03a0\\u03c1\\u03b1\\u03c3\\u03c3\\u03ac-\\u039b\\u03b9\\u03bc\\u03ac\\u03bd\\u03b9-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/prassa-limani-tombolo\\\/\\\">Prassa Limani Tombolo<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/prassa-limani-tombolo\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The \\\"Prasa Limani\\\" Tombolo, found on the northern side of the Agios Ioannis beach, is the sandy path that links the volcanic rock to the shore. Rising magma penetrated and solidified in\\u00a0pre-existing volcanic rocks and\\u00a0formed\\u00a0the islet. Over time, erosion removed the surrounding rocks, exposing the volcanic vein. The tombolo is a coastal deposition formation composed [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.927\",\"lng\":\"25.067\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/prassa-limani-tombolo\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The \\\"Prasa Limani\\\" Tombolo, found on the northern side of the Agios Ioannis beach, is the sandy path that links the volcanic rock to the shore. Rising magma penetrated and solidified in\\u00a0pre-existing volcanic rocks and\\u00a0formed\\u00a0the islet. Over time, erosion removed the surrounding rocks, exposing the volcanic vein. 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The formation of a tombolo is formed by the impact of sea waves and the restriction of their transport capacity, which results in materials such as sand and pebbles collecting there, eventually producing a strip of land that connects the island to the nearby shore.\\r\\n\\r\\n<\\\/div>\",\"post_title\":\"Prassa Limani Tombolo\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/prassa-limani-tombolo\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Prassa Limani Tombolo\\\" width=\\\"300\\\" height=\\\"210\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/4-\\u03a4\\u03cc\\u03bc\\u03c0\\u03bf\\u03bb\\u03bf-\\u03a0\\u03c1\\u03b1\\u03c3\\u03c3\\u03ac-\\u039b\\u03b9\\u03bc\\u03ac\\u03bd\\u03b9-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.927\",\"%wpcf-longtitude%\":\"25.067\",\"%wpcf-location%\":\"\\u0386\\u03b3\\u03b9\\u03bf\\u03c2 \\u0399\\u03c9\\u03ac\\u03bd\\u03bd\\u03b7\\u03c2\",\"%_wpgmp_metabox_latitude%\":\"39.927\",\"%_wpgmp_metabox_longitude%\":\"25.067\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"14\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi.png\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2751\",\"%_edit_lock%\":\"1655279427:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%84%cf%8c%ce%bc%cf%80%ce%bf%ce%bb%ce%bf-%ce%b1%ce%b3%ce%af%ce%bf%cf%85-%ce%b9%cf%89%ce%ac%ce%bd%ce%bd%ce%b7\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/4-\\u03a4\\u03cc\\u03bc\\u03c0\\u03bf\\u03bb\\u03bf-\\u03a0\\u03c1\\u03b1\\u03c3\\u03c3\\u03ac-\\u039b\\u03b9\\u03bc\\u03ac\\u03bd\\u03b9.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20282\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/4-\\u03a4\\u03cc\\u03bc\\u03c0\\u03bf\\u03bb\\u03bf-\\u03a0\\u03c1\\u03b1\\u03c3\\u03c3\\u03ac-\\u039b\\u03b9\\u03bc\\u03ac\\u03bd\\u03b9.jpg, 4-\\u03a4\\u03cc\\u03bc\\u03c0\\u03bf\\u03bb\\u03bf \\u03a0\\u03c1\\u03b1\\u03c3\\u03c3\\u03ac \\u039b\\u03b9\\u03bc\\u03ac\\u03bd\\u03b9, \",\"%_et_pb_truncate_post%\":\"<p>The &#8220;Prasa Limani&#8221; Tombolo, found on the northern side of the Agios Ioannis beach, is the sandy path that links the volcanic rock to the shore.<\\\/p>\\n<p>Rising magma penetrated and solidified in\\u00a0pre-existing volcanic rocks and\\u00a0formed\\u00a0the islet. 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geosites\"},\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\"},\"id\":3586,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\",\"name\":\"\\u03a0\\u03b1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b9\\u03bf\\u03b9\",\"id\":\"14\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"St. Efthimia Tombolo\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"St. Efthimia Tombolo\\\" width=\\\"300\\\" height=\\\"210\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/13-\\u03a4\\u03cc\\u03bc\\u03c0\\u03bf\\u03bb\\u03bf-\\u0391\\u03b3\\u03af\\u03b1\\u03c2-\\u0395\\u03c5\\u03b8\\u03c5\\u03bc\\u03af\\u03b1\\u03c2-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/st-efthimia-tombolo\\\/\\\">St. Efthimia Tombolo<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/st-efthimia-tombolo\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The tombolo of St. Efthimia is located south of Lemnos, on the southwest shore of Cape \\\"Fakos\\\". The tombolo is a natural corridor composed of loose sediments that links the coast to the neighboring rocky islet. After being cut off from the nearby shore, the islet operated as a seawall, causing the sea waves to [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.809040\",\"lng\":\"25.141208\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/st-efthimia-tombolo\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The tombolo of St. Efthimia is located south of Lemnos, on the southwest shore of Cape \\\"Fakos\\\". The tombolo is a natural corridor composed of loose sediments that links the coast to the neighboring rocky islet. After being cut off from the nearby shore, the islet operated as a seawall, causing the sea waves to [&hellip;]<\\\/p>\\n\",\"post_content\":\"The tombolo of St. Efthimia is located south of Lemnos, on the southwest shore of Cape \\\"Fakos\\\". The tombolo is a natural corridor composed of loose sediments that links the coast to the neighboring rocky islet.\\r\\n\\r\\nAfter being cut off from the nearby shore, the islet operated as a seawall, causing the sea waves to lose their carrying capacity and deposit the sediments they carried.\\r\\n\\r\\nThe land strip was formed over time by the constant deposition of sediment from the sea waves, and visitors may observe and stroll on it as well as visit the charming church of St. Efthimia.\",\"post_title\":\"St. Efthimia Tombolo\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/st-efthimia-tombolo\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"St. Efthimia Tombolo\\\" width=\\\"300\\\" height=\\\"210\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/13-\\u03a4\\u03cc\\u03bc\\u03c0\\u03bf\\u03bb\\u03bf-\\u0391\\u03b3\\u03af\\u03b1\\u03c2-\\u0395\\u03c5\\u03b8\\u03c5\\u03bc\\u03af\\u03b1\\u03c2-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.809040\",\"%wpcf-longtitude%\":\"25.141208\",\"%wpcf-location%\":\"\\u0391\\u03ba\\u03c1\\u03c9\\u03c4\\u03ae\\u03c1\\u03b9 \\u0391\\u03b3\\u03af\\u03b1\\u03c2 \\u0395\\u03c5\\u03b8\\u03c5\\u03bc\\u03af\\u03b1\\u03c2 (\\u03a3\\u03c4\\u03b1\\u03c5\\u03c1\\u03cc\\u03c2) \\u03a6\\u03b1\\u03ba\\u03cc\\u03c2\",\"%_wpgmp_metabox_latitude%\":\"39.809040\",\"%_wpgmp_metabox_longitude%\":\"25.141208\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"14\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi.png\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2760\",\"%_edit_lock%\":\"1655280669:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%84%cf%8c%ce%bc%cf%80%ce%bf%ce%bb%ce%bf-%ce%b1%ce%b3%ce%af%ce%b1%cf%82-%ce%b5%cf%85%ce%b8%cf%85%ce%bc%ce%af%ce%b1%cf%82\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/13-\\u03a4\\u03cc\\u03bc\\u03c0\\u03bf\\u03bb\\u03bf-\\u0391\\u03b3\\u03af\\u03b1\\u03c2-\\u0395\\u03c5\\u03b8\\u03c5\\u03bc\\u03af\\u03b1\\u03c2.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20318\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/13-\\u03a4\\u03cc\\u03bc\\u03c0\\u03bf\\u03bb\\u03bf-\\u0391\\u03b3\\u03af\\u03b1\\u03c2-\\u0395\\u03c5\\u03b8\\u03c5\\u03bc\\u03af\\u03b1\\u03c2.jpg, 13-\\u03a4\\u03cc\\u03bc\\u03c0\\u03bf\\u03bb\\u03bf \\u0391\\u03b3\\u03af\\u03b1\\u03c2 \\u0395\\u03c5\\u03b8\\u03c5\\u03bc\\u03af\\u03b1\\u03c2, \",\"%_et_pb_truncate_post%\":\"<p>The tombolo of St. Efthimia is located south of Lemnos, on the southwest shore of Cape &#8220;Fakos&#8221;. 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geosites\"},\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\"},\"id\":3588,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\",\"name\":\"\\u03a0\\u03b1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b9\\u03bf\\u03b9\",\"id\":\"14\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Pournias Erosion Formations\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Pournias Erosion Formations\\\" width=\\\"300\\\" height=\\\"164\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/26-\\u0391\\u03ba\\u03c1\\u03c9\\u03c4\\u03ae\\u03c1\\u03b9\\u03bf-\\u03a0\\u03bf\\u03c5\\u03c1\\u03bd\\u03b9\\u03ac-\\u03b3\\u03b5\\u03c9\\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2-\\u03b4\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-2-scaled-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/pournias-erosion-formations\\\/\\\">Pournias Erosion Formations<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/pournias-erosion-formations\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The impressive Pournias coastal erosion formations are visible in the thick layered sandstone and conglomerate rocks of northern Lemnos, west of Cape Pournia. The area is covered with sedimentary geological formations from Upper Eocene-Lower Oligocene deposited in underwater channels 27-33 million years ago. Honeycomb and spheroidal types of weathering have been observed in the area. [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.951\",\"lng\":\"25.287\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/pournias-erosion-formations\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The impressive Pournias coastal erosion formations are visible in the thick layered sandstone and conglomerate rocks of northern Lemnos, west of Cape Pournia. The area is covered with sedimentary geological formations from Upper Eocene-Lower Oligocene deposited in underwater channels 27-33 million years ago. Honeycomb and spheroidal types of weathering have been observed in the area. [&hellip;]<\\\/p>\\n\",\"post_content\":\"The impressive Pournias coastal erosion formations are visible in the thick layered sandstone and conglomerate rocks of northern Lemnos, west of Cape Pournia.\\r\\n\\r\\nThe area is covered with sedimentary geological formations from Upper Eocene-Lower Oligocene deposited in underwater channels 27-33 million years ago.\\r\\n\\r\\nHoneycomb and spheroidal types of weathering have been observed in the area. This is the result of the differential erosion of the sandstone rocks, caused by the structure of the rock which creates weak areas on its surface which are affected by sea waves and salt deposited by sea spray. This process results in impressive and complicated formations in the rocks.\",\"post_title\":\"Pournias Erosion Formations\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/pournias-erosion-formations\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Pournias Erosion Formations\\\" width=\\\"300\\\" height=\\\"164\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/26-\\u0391\\u03ba\\u03c1\\u03c9\\u03c4\\u03ae\\u03c1\\u03b9\\u03bf-\\u03a0\\u03bf\\u03c5\\u03c1\\u03bd\\u03b9\\u03ac-\\u03b3\\u03b5\\u03c9\\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2-\\u03b4\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-2-scaled-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.951\",\"%wpcf-longtitude%\":\"25.287\",\"%wpcf-location%\":\"\\u0391\\u03ba. \\u03a0\\u03bf\\u03c5\\u03c1\\u03bd\\u03b9\\u03ac\",\"%_wpgmp_metabox_latitude%\":\"39.951\",\"%_wpgmp_metabox_longitude%\":\"25.287\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"14\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi.png\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"3001\",\"%_edit_lock%\":\"1655281531:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%bc%ce%bf%cf%81%cf%86%ce%ad%cf%82-%ce%b4%ce%b9%ce%ac%ce%b2%cf%81%cf%89%cf%83%ce%b7%cf%82-%ce%b1%ce%ba%cf%81%cf%89%cf%84%ce%b7%cf%81%ce%af%ce%bf%cf%85-%cf%80%ce%bf%cf%85%cf%81%ce%bd%ce%b9%ce%ac\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/26-\\u0391\\u03ba\\u03c1\\u03c9\\u03c4\\u03ae\\u03c1\\u03b9\\u03bf-\\u03a0\\u03bf\\u03c5\\u03c1\\u03bd\\u03b9\\u03ac-\\u03b3\\u03b5\\u03c9\\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2-\\u03b4\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-2.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20359, 20360, 20361, 20362, 20363, 20364\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/pournias3.jpg, pournias3, \",\"%_et_pb_truncate_post%\":\"<p>The impressive Pournias coastal erosion formations are visible in the thick layered sandstone and conglomerate rocks of northern Lemnos, west of Cape Pournia.<\\\/p>\\n<p>The area is covered with sedimentary geological formations from Upper Eocene-Lower Oligocene deposited in underwater channels 27-33 million years ago.<\\\/p>\\n<p>Honeycomb and spheroidal types of weathering have been observed in the area. 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src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/5-\\u03a0\\u03b1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b9\\u03b5\\u03c2-\\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2-\\u03b4\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-\\u0391\\u03b3\\u03af\\u03bf\\u03c5-\\u0399\\u03c9\\u03ac\\u03bd\\u03bd\\u03b7-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/coastal-erosion-formations-of-st-ioannis\\\/\\\">Coastal Erosion Formations of St. Ioannis<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/coastal-erosion-formations-of-st-ioannis\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The coastal columnar formations (stacks) northwest of Kaspakas on the beach of Agios Ioannis are geoforms formed by the sea eroding pyroclastic formations caused by intense volcanic activity during the Lower Miocene. Coastal columns formations (stacks) refer to rock formations that rise above sea level along rocky beaches. They occur as a result of the [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.9248\",\"lng\":\"25.0673676\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/coastal-erosion-formations-of-st-ioannis\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The coastal columnar formations (stacks) northwest of Kaspakas on the beach of Agios Ioannis are geoforms formed by the sea eroding pyroclastic formations caused by intense volcanic activity during the Lower Miocene. Coastal columns formations (stacks) refer to rock formations that rise above sea level along rocky beaches. They occur as a result of the [&hellip;]<\\\/p>\\n\",\"post_content\":\"<div class=\\\"sections__field-body\\\">\\r\\n\\r\\nThe coastal columnar formations (stacks) northwest of Kaspakas on the beach of Agios Ioannis are geoforms formed by the sea eroding pyroclastic formations caused by intense volcanic activity during the Lower Miocene.\\r\\n\\r\\nCoastal columns formations (stacks) refer to rock formations that rise above sea level along rocky beaches. They occur as a result of the strong differential erosion of a rocky beach by the sea waves and wind.\\r\\n\\r\\nThe definition \\\"stack\\\" is derived from the word \\\"stakkur\\\" which is the Scandinavian dialect of the Faeroe Islands, where these coastal formations are common along the high, steep, and rocky beaches.\\r\\n\\r\\n<\\\/div>\",\"post_title\":\"Coastal Erosion Formations of St. Ioannis\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/coastal-erosion-formations-of-st-ioannis\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Coastal Erosion Formations of St. Ioannis\\\" width=\\\"300\\\" height=\\\"209\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/5-\\u03a0\\u03b1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b9\\u03b5\\u03c2-\\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2-\\u03b4\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-\\u0391\\u03b3\\u03af\\u03bf\\u03c5-\\u0399\\u03c9\\u03ac\\u03bd\\u03bd\\u03b7-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.9248\",\"%wpcf-longtitude%\":\"25.0673676\",\"%wpcf-location%\":\"\\u039a\\u03ac\\u03c3\\u03c0\\u03b1\\u03ba\\u03b1\\u03c2, \\u0386\\u03b3\\u03b9\\u03bf\\u03c2 \\u0399\\u03c9\\u03ac\\u03bd\\u03bd\\u03b7\\u03c2\",\"%_wpgmp_metabox_latitude%\":\"39.9248\",\"%_wpgmp_metabox_longitude%\":\"25.0673676\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"14\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi.png\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2750\",\"%_edit_lock%\":\"1655283054:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%80%ce%b1%cf%81%ce%ac%ce%ba%cf%84%ce%b9%ce%b5%cf%82-%ce%b4%ce%bf%ce%bc%ce%ad%cf%82-%ce%b4%ce%b9%ce%ac%ce%b2%cf%81%cf%89%cf%83%ce%b7%cf%82-%ce%b1%ce%b3%ce%af%ce%bf%cf%85-%ce%b9%cf%89%ce%ac%ce%bd\",\"%wpcf-image-gallery%\":\"\",\"%_wpcf-image-gallery-sort-order%\":\"20402\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/5-\\u03a0\\u03b1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b9\\u03b5\\u03c2-\\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2-\\u03b4\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2-\\u0391\\u03b3\\u03af\\u03bf\\u03c5-\\u0399\\u03c9\\u03ac\\u03bd\\u03bd\\u03b7.jpg, 5-\\u03a0\\u03b1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b9\\u03b5\\u03c2 \\u03bc\\u03bf\\u03c1\\u03c6\\u03ad\\u03c2 \\u03b4\\u03b9\\u03ac\\u03b2\\u03c1\\u03c9\\u03c3\\u03b7\\u03c2 \\u0391\\u03b3\\u03af\\u03bf\\u03c5 \\u0399\\u03c9\\u03ac\\u03bd\\u03bd\\u03b7, \",\"%_et_pb_truncate_post%\":\"<p>The coastal columnar formations (stacks) northwest of Kaspakas on the beach of Agios Ioannis are geoforms formed by the sea eroding pyroclastic formations caused by intense volcanic activity during the Lower Miocene.<\\\/p>\\n<p>Coastal columns formations (stacks) refer to rock formations that rise above sea level along rocky beaches. 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geosites\"},\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\"},\"id\":3592,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi_sm-small.png\",\"name\":\"\\u03a0\\u03b1\\u03c1\\u03ac\\u03ba\\u03c4\\u03b9\\u03bf\\u03b9\",\"id\":\"14\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Louri Beach Erosion Formations\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Louri Beach Erosion Formations\\\" width=\\\"300\\\" height=\\\"209\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/49-\\u03a0\\u03b1\\u03c1\\u03b1\\u03bb\\u03af\\u03b1-\\u039b\\u03bf\\u03c5\\u03c1\\u03af-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/louri-beach-erosion-formations\\\/\\\">Louri Beach Erosion Formations<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/louri-beach-erosion-formations\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Louri beach is located near of the southeastern coast of Lemnos, to the east of the town of Skandali and distinguished by an intense folding of 33 million-year-old sandstone rocks. The layers of sandstone rocks curve and create a 90-degree angle along the Louri beach. This curve is caused due to the shear stresses caused [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.795656\",\"lng\":\"25.350254\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/louri-beach-erosion-formations\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Louri beach is located near of the southeastern coast of Lemnos, to the east of the town of Skandali and distinguished by an intense folding of 33 million-year-old sandstone rocks. The layers of sandstone rocks curve and create a 90-degree angle along the Louri beach. This curve is caused due to the shear stresses caused [&hellip;]<\\\/p>\\n\",\"post_content\":\"<div class=\\\"sections__field-body\\\">\\r\\n<div class=\\\"sections__field-body\\\">\\r\\n\\r\\nLouri beach is located near of the southeastern coast of Lemnos, to the east of the town of Skandali and distinguished by an intense folding of 33 million-year-old sandstone rocks.\\r\\n\\r\\nThe layers of sandstone rocks curve and create a 90-degree angle along the Louri beach. This curve is caused due to the shear stresses caused by the activation of large faults.\\r\\n\\r\\nIn these sandstone layers can be found impressive honeycomb weathering shapes, formed by the wind, waves and sea spray.\\r\\n\\r\\nClose by there are also sand dunes formed by the deposition of products from the erosion of sandstone rocks.\\r\\n\\r\\n<\\\/div>\\r\\n<\\\/div>\",\"post_title\":\"Louri Beach Erosion Formations\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/louri-beach-erosion-formations\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Louri Beach Erosion Formations\\\" width=\\\"300\\\" height=\\\"209\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/49-\\u03a0\\u03b1\\u03c1\\u03b1\\u03bb\\u03af\\u03b1-\\u039b\\u03bf\\u03c5\\u03c1\\u03af-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.795656\",\"%wpcf-longtitude%\":\"25.350254\",\"%wpcf-location%\":\"\\u03a0\\u03b1\\u03c1\\u03b1\\u03bb\\u03af\\u03b1 \\u039b\\u03bf\\u03c5\\u03c1\\u03af\",\"%_wpgmp_metabox_latitude%\":\"39.795656\",\"%_wpgmp_metabox_longitude%\":\"25.350254\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:2:\\\"14\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2022\\\/02\\\/paraktioi.png\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_thumbnail_id%\":\"2735\",\"%_edit_lock%\":\"1655288061:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%80%ce%b1%cf%81%ce%b1%ce%bb%ce%af%ce%b1-%ce%bb%ce%bf%cf%85%cf%81%ce%af\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/49-\\u03a0\\u03b1\\u03c1\\u03b1\\u03bb\\u03af\\u03b1-\\u039b\\u03bf\\u03c5\\u03c1\\u03af.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20444\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/49-\\u03a0\\u03b1\\u03c1\\u03b1\\u03bb\\u03af\\u03b1-\\u039b\\u03bf\\u03c5\\u03c1\\u03af.jpg, 49-\\u03a0\\u03b1\\u03c1\\u03b1\\u03bb\\u03af\\u03b1 \\u039b\\u03bf\\u03c5\\u03c1\\u03af, \",\"%_et_pb_truncate_post%\":\"<p>Louri beach is located near of the southeastern coast of Lemnos, to the east of the town of Skandali and distinguished by an intense folding of 33 million-year-old sandstone rocks.<\\\/p>\\n<p>The layers of sandstone rocks curve and create a 90-degree angle along the Louri beach. 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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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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. 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","protected":false},"author":2,"featured_media":2750,"parent":3202,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_et_pb_use_builder":"on","_et_pb_old_content":"","_et_gb_content_width":"","footnotes":""},"_links":{"self":[{"href":"https:\/\/www.lemnosgeomonuments.gr\/en\/wp-json\/wp\/v2\/pages\/3258"}],"collection":[{"href":"https:\/\/www.lemnosgeomonuments.gr\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.lemnosgeomonuments.gr\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.lemnosgeomonuments.gr\/en\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.lemnosgeomonuments.gr\/en\/wp-json\/wp\/v2\/comments?post=3258"}],"version-history":[{"count":5,"href":"https:\/\/www.lemnosgeomonuments.gr\/en\/wp-json\/wp\/v2\/pages\/3258\/revisions"}],"predecessor-version":[{"id":3540,"href":"https:\/\/www.lemnosgeomonuments.gr\/en\/wp-json\/wp\/v2\/pages\/3258\/revisions\/3540"}],"up":[{"embeddable":true,"href":"https:\/\/www.lemnosgeomonuments.gr\/en\/wp-json\/wp\/v2\/pages\/3202"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.lemnosgeomonuments.gr\/en\/wp-json\/wp\/v2\/media\/2750"}],"wp:attachment":[{"href":"https:\/\/www.lemnosgeomonuments.gr\/en\/wp-json\/wp\/v2\/media?parent=3258"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}