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_builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; global_colors_info=&#8221;{}&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_text module_class=&#8221;downMenu&#8221; _builder_version=&#8221;4.11.4&#8243; _dynamic_attributes=&#8221;link_option_url&#8221; text_font=&#8221;|700|||||||&#8221; text_text_color=&#8221;#FFFFFF&#8221; text_font_size=&#8221;15px&#8221; text_letter_spacing=&#8221;2px&#8221; header_text_color=&#8221;#FFFFFF&#8221; header_2_font=&#8221;||||||||&#8221; background_color=&#8221;#034b6b&#8221; text_orientation=&#8221;center&#8221; background_layout=&#8221;dark&#8221; custom_margin=&#8221;0px||||false|false&#8221; 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; custom_padding__hover=&#8221;|||&#8221;][et_pb_text module_class=&#8221;downMenu&#8221; _builder_version=&#8221;4.11.4&#8243; _dynamic_attributes=&#8221;link_option_url&#8221; text_font=&#8221;|700|||||||&#8221; text_text_color=&#8221;#FFFFFF&#8221; text_font_size=&#8221;15px&#8221; text_letter_spacing=&#8221;2px&#8221; header_text_color=&#8221;#FFFFFF&#8221; header_2_font=&#8221;||||||||&#8221; background_color=&#8221;#034b6b&#8221; text_orientation=&#8221;center&#8221; background_layout=&#8221;dark&#8221; custom_margin=&#8221;0px||||false|false&#8221; custom_padding=&#8221;30px|20px|30px|20px|true|true&#8221; link_option_url=&#8221;@ET-DC@eyJkeW5hbWljIjp0cnVlLCJjb250ZW50IjoicG9zdF9saW5rX3VybF9wYWdlIiwic2V0dGluZ3MiOnsicG9zdF9pZCI6IjE3MjEifX0=@&#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>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;29px||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;4.9.7&#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>&nbsp;<\/p>\n<p><strong>Weathering &#8211; Erosion geoforms<br \/><\/strong><\/p>\n<p>For millions of years, the persistent activity of water, air, and waves has sculpted the rocks of Lemnos island, from large tafoni, found in the volcanic rocks to the west, to spheroidal weathering formations on the sandstone rocks on the island&#8217;s northern and northeastern shores.<\/p>\n<p>Erosion geoforms are areas in which the activity of chemical and physical weathering, as well as the erosion of Lemnos&#8217; volcanic and sedimentary rocks, creates spectacular formations in the terrain. Remarkable shapes in the terrain intrigue visitors to explore and enjoy these impressive works of nature up close.<\/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; max_width=&#8221;80px&#8221; height=&#8221;3px&#8221; locked=&#8221;off&#8221; global_colors_info=&#8221;{}&#8221;]<br \/>\n[\/et_pb_divider][et_pb_dpfilterable_blog posts_number=&#8221;30&#8243; custom_post_types=&#8221;simeio&#8221; include_categories=&#8221;4&#8243; hide_all=&#8221;on&#8221; fullwidth=&#8221;off&#8221; zoom_icon_color=&#8221;#00140b&#8221; hover_overlay_color=&#8221;rgba(165,186,178,0.8)&#8221; _builder_version=&#8221;4.11.4&#8243; _module_preset=&#8221;default&#8221; custom_margin=&#8221;||6px|||&#8221; custom_css_portfolio_filters=&#8221;display:none;&#8221; global_colors_info=&#8221;{}&#8221;][\/et_pb_dpfilterable_blog][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=&#8221;1&#8243; disabled_on=&#8221;off|off|off&#8221; admin_label=&#8221;Events&#8221; _builder_version=&#8221;4.9.7&#8243; background_color=&#8221;#a5bab2&#8243; custom_padding=&#8221;21px||0|0px|false|false&#8221; custom_width_px__hover=&#8221;1080px&#8221; custom_width_px__hover_enabled=&#8221;1080px&#8221; custom_width_percent__hover=&#8221;80%&#8221; custom_width_percent__hover_enabled=&#8221;80%&#8221; 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; background_color_gradient_overlays_image__hover_enabled=&#8221;off&#8221; parallax__hover=&#8221;off&#8221; parallax__hover_enabled=&#8221;off&#8221; parallax_method__hover=&#8221;on&#8221; parallax_method__hover_enabled=&#8221;on&#8221; background_size__hover=&#8221;cover&#8221; background_size__hover_enabled=&#8221;cover&#8221; background_position__hover=&#8221;center&#8221; background_position__hover_enabled=&#8221;center&#8221; background_repeat__hover=&#8221;no-repeat&#8221; background_repeat__hover_enabled=&#8221;no-repeat&#8221; background_blend__hover=&#8221;normal&#8221; background_blend__hover_enabled=&#8221;normal&#8221; allow_player_pause__hover=&#8221;off&#8221; allow_player_pause__hover_enabled=&#8221;off&#8221; background_video_pause_outside_viewport__hover=&#8221;on&#8221; 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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; filter_brightness__hover=&#8221;100%&#8221; filter_brightness__hover_enabled=&#8221;100%&#8221; filter_contrast__hover=&#8221;100%&#8221; filter_contrast__hover_enabled=&#8221;100%&#8221; filter_invert__hover=&#8221;0%&#8221; filter_invert__hover_enabled=&#8221;0%&#8221; filter_sepia__hover=&#8221;0%&#8221; filter_sepia__hover_enabled=&#8221;0%&#8221; filter_opacity__hover=&#8221;100%&#8221; filter_opacity__hover_enabled=&#8221;100%&#8221; filter_blur__hover=&#8221;0px&#8221; filter_blur__hover_enabled=&#8221;0px&#8221; mix_blend_mode__hover=&#8221;normal&#8221; mix_blend_mode__hover_enabled=&#8221;normal&#8221; animation_style__hover=&#8221;none&#8221; animation_style__hover_enabled=&#8221;none&#8221; animation_repeat__hover=&#8221;once&#8221; animation_repeat__hover_enabled=&#8221;once&#8221; animation_direction__hover=&#8221;center&#8221; animation_direction__hover_enabled=&#8221;center&#8221; animation_duration__hover=&#8221;1000ms&#8221; 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; global_colors_info=&#8221;{}&#8221;][et_pb_text _builder_version=&#8221;4.11.4&#8243; text_font=&#8221;||||||||&#8221; header_font=&#8221;||||||||&#8221; header_text_color=&#8221;#004235&#8243; header_2_font=&#8221;Noto Serif||||||||&#8221; header_2_font_size=&#8221;40px&#8221; header_2_line_height=&#8221;1.4em&#8221; header_3_text_align=&#8221;center&#8221; header_3_text_color=&#8221;#FFFFFF&#8221; text_orientation=&#8221;center&#8221; background_layout=&#8221;dark&#8221; custom_margin=&#8221;-23px||8px|||&#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 on map<\/h3>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column 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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. 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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 erosion.<\\\/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\":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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\\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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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. 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":1,"featured_media":0,"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\/3256"}],"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\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.lemnosgeomonuments.gr\/en\/wp-json\/wp\/v2\/comments?post=3256"}],"version-history":[{"count":5,"href":"https:\/\/www.lemnosgeomonuments.gr\/en\/wp-json\/wp\/v2\/pages\/3256\/revisions"}],"predecessor-version":[{"id":3632,"href":"https:\/\/www.lemnosgeomonuments.gr\/en\/wp-json\/wp\/v2\/pages\/3256\/revisions\/3632"}],"up":[{"embeddable":true,"href":"https:\/\/www.lemnosgeomonuments.gr\/en\/wp-json\/wp\/v2\/pages\/3202"}],"wp:attachment":[{"href":"https:\/\/www.lemnosgeomonuments.gr\/en\/wp-json\/wp\/v2\/media?parent=3256"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}