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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;||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><strong>Tectonic Geosites<br \/><\/strong><\/p>\n<p>Tectonic processes have actively and significantly shaped the landscape of Lemnos Island. Large, ruptured structures that run the width and length of the island have fragmented the coasts and given Lemnos its current &#8220;shape&#8221;.<\/p>\n<p>Serving as impressive sites of geological interest found in a variety of locations on Lemnos, these tectonic geosites shed light on the evolution of the earth\u2019s crust to create its current form. The most impressive of these geosites is the Kaspakas fault.<\/p>\n<p>Large impressive faults that build intense terrain and secondary geoforms like waterfalls demonstrate the force of the processes that sculpt the Earth&#8217;s crust.<\/p>\n<p>&nbsp;<\/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 custom_post_types=&#8221;simeio&#8221; include_categories=&#8221;3&#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; disabled_on=&#8221;off|off|off&#8221; _builder_version=&#8221;4.11.3&#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; 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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; 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allow_player_pause__hover_enabled=&#8221;off&#8221; background_video_pause_outside_viewport__hover=&#8221;on&#8221; background_video_pause_outside_viewport__hover_enabled=&#8221;on&#8221; inner_shadow__hover=&#8221;off&#8221; inner_shadow__hover_enabled=&#8221;off&#8221; make_fullwidth__hover=&#8221;off&#8221; 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; 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 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     <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kaspakas-fault\\\/\\\">Kaspakas Fault<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kaspakas-fault\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The Kaspakas active fault appears north of the Kaspakas village. The fault is visible as a morphological rise in the hills east of the village. It is a large tectonic surface with a length of 11 km and a direction of NW-SE that was caused by recent seismic activity in the area that led the [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.935\",\"lng\":\"25.068\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kaspakas-fault\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The Kaspakas active fault appears north of the Kaspakas village. The fault is visible as a morphological rise in the hills east of the village. It is a large tectonic surface with a length of 11 km and a direction of NW-SE that was caused by recent seismic activity in the area that led the [&hellip;]<\\\/p>\\n\",\"post_content\":\"The Kaspakas active fault appears north of the Kaspakas village. The fault is visible as a morphological rise in the hills east of the village. It is a large tectonic surface with a length of 11 km and a direction of NW-SE that was caused by recent seismic activity in the area that led the rock to break.\\r\\n\\r\\nFaults are geological structures formed when strain in the Earth\\u2019s crust exceed the limit of rock strength, forcing it to break. The evidence of rock movement appears on the surface of the fault as scratches which are referred to as slip lines. These lines are critical for understanding the fault\\u2019s seismic activity.\\r\\n\\r\\nThe Kaspakas fault links rock formations of different ages together, specifically volcanic rocks (Upper Oligocene \\u2013 Middle Miocene) and Molassic sediments (Eocene).\",\"post_title\":\"Kaspakas Fault\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kaspakas-fault\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Kaspakas Fault\\\" width=\\\"300\\\" height=\\\"225\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/2-\\u03a1\\u03ae\\u03b3\\u03bc\\u03b1-\\u039a\\u03ac\\u03c3\\u03c0\\u03b1\\u03ba\\u03b1-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.935\",\"%wpcf-longtitude%\":\"25.068\",\"%wpcf-location%\":\"\\u039a\\u03ac\\u03c3\\u03c0\\u03b1\\u03ba\\u03b1\",\"%_wpgmp_metabox_latitude%\":\"39.935\",\"%_wpgmp_metabox_longitude%\":\"25.068\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"5\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/tectonic.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%wpcf-code%\":\"\",\"%_wpml_location_migration_done%\":\"1\",\"%_wpml_word_count%\":\"{\\\"total\\\":149,\\\"to_translate\\\":{\\\"en\\\":149}}\",\"%_thumbnail_id%\":\"2753\",\"%_edit_lock%\":\"1655206720:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%81%ce%ae%ce%b3%ce%bc%ce%b1-%ce%ba%ce%ac%cf%83%cf%80%ce%b1%ce%ba%ce%b1\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/2-\\u03a1\\u03ae\\u03b3\\u03bc\\u03b1-\\u039a\\u03ac\\u03c3\\u03c0\\u03b1\\u03ba\\u03b1.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"19834, 19835\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/2-\\u03ba\\u03ac\\u03c3\\u03c0\\u03b1\\u03ba\\u03b1\\u03c2-scaled.jpg, 2-\\u03ba\\u03ac\\u03c3\\u03c0\\u03b1\\u03ba\\u03b1\\u03c2, \",\"%_et_pb_truncate_post%\":\"<p>The Kaspakas active fault appears north of the Kaspakas village. The fault is visible as a morphological rise in the hills east of the village. It is a large tectonic surface with a length of 11 km and a direction of NW-SE that was caused by recent seismic activity in the area that led the rock to break.<\\\/p>\\n<p>Faults are geological structures formed when strain in the Earth\\u2019s crust exceed the limit of rock strength, forcing it to break. The evidence of rock movement appears on the surface of the fault as scratches which are referred to as slip lines. 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geosites\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/tectonic_result-small.png\"},\"id\":3569,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/tectonic_result-small.png\",\"name\":\"\\u03a4\\u03b5\\u03ba\\u03c4\\u03bf\\u03bd\\u03b9\\u03ba\\u03bf\\u03af\",\"id\":\"5\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"St. Charalambos Plakas Fault\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"St. Charalambos Plakas Fault\\\" width=\\\"300\\\" height=\\\"221\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/35-\\u0386\\u03b3\\u03b9\\u03bf\\u03c2-\\u03a7\\u03b1\\u03c1\\u03ac\\u03bb\\u03b1\\u03bc\\u03c0\\u03bf\\u03c2-\\u03a0\\u03bb\\u03ac\\u03ba\\u03b1\\u03c2-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding 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A large fault cuts through the area\\u2019s geological layers of sedimentary rocks. It is a normal fault with a NW-SE direction. The fault runs along the beach, right next to [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"40.0198\",\"lng\":\"25.4164\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/st-charalambos-plakas-fault\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Alterations of sandstone and clay geological formations, typical of Lemnos\\u2019s molassic deposits, are found northwest of the Plaka settlement, in the area of Saint Charalambos. A large fault cuts through the area\\u2019s geological layers of sedimentary rocks. It is a normal fault with a NW-SE direction. The fault runs along the beach, right next to [&hellip;]<\\\/p>\\n\",\"post_content\":\"Alterations of sandstone and clay geological formations, typical of Lemnos\\u2019s molassic deposits, are found northwest of the Plaka settlement, in the area of Saint Charalambos. A large fault cuts through the area\\u2019s geological layers of sedimentary rocks.\\r\\n\\r\\nIt is a normal fault with a NW-SE direction. The fault runs along the beach, right next to the steps leading down to the church\\u2019s holy water, where the movement of the geological formations on the vertical slope may be seen.\\r\\n\\r\\nThe evidence of rock movement is visible on the surface of the fault as fractures known as striations. These tectonic lines were formed by the friction of the rocks in their parallel movement and provide crucial information about the fault\\u2019s seismic activity in the past.\",\"post_title\":\"St. Charalambos Plakas Fault\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/st-charalambos-plakas-fault\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"St. Charalambos Plakas Fault\\\" width=\\\"300\\\" height=\\\"221\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/35-\\u0386\\u03b3\\u03b9\\u03bf\\u03c2-\\u03a7\\u03b1\\u03c1\\u03ac\\u03bb\\u03b1\\u03bc\\u03c0\\u03bf\\u03c2-\\u03a0\\u03bb\\u03ac\\u03ba\\u03b1\\u03c2-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" 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Clays and sandstones with interstitial cobblestones (rock with rounded pebbles within) in the lower layers, aged about 23 [&hellip;]<\\\/p>\\n\",\"address\":\"V83X+XH \\u039c\\u03bf\\u03cd\\u03b4\\u03c1\\u03bf\\u03c2, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.854896914322005\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.34899999734496\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/poliochni-harbour-fault\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The stratigraphic contact of two separate geological formations, particularly the upper molassic sediments of Lemnos and the pyroclastic formations of Romanos, is located north of the ancient site of Poliochni on the slopes of the scenic harbor. Clays and sandstones with interstitial cobblestones (rock with rounded pebbles within) in the lower layers, aged about 23 [&hellip;]<\\\/p>\\n\",\"post_content\":\"The stratigraphic contact of two separate geological formations, particularly the upper molassic sediments of Lemnos and the pyroclastic formations of Romanos, is located north of the ancient site of Poliochni on the slopes of the scenic harbor. Clays and sandstones with interstitial cobblestones (rock with rounded pebbles within) in the lower layers, aged about 23 million years, can be found with a general dip direction to the NW under the Lower Miocene tuff.\\r\\n\\r\\nMarine sedimentogenesis occurred between 22 and 28 million years ago, resulting in the sedimentary formations of Lemnos. Around 22 million years ago, the earliest volcanic products of Lemnos, pyroclastic rocks with layers of volcanic ash with various rock fragments, settled over these sedimentary rocks.\\r\\n\\r\\nAt this location, the movement of tectonic faults in the NE-SW direction alters the layers and brings older sedimentary formations into contact with younger volcanic formations, resulting in a complicated geological picture.\",\"post_title\":\"Poliochni (harbour) Fault\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/poliochni-harbour-fault\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Poliochni (harbour) Fault\\\" width=\\\"300\\\" height=\\\"209\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/46-\\u03a0\\u03bf\\u03bb\\u03b9\\u03cc\\u03c7\\u03bd\\u03b7-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.85489\",\"%wpcf-longtitude%\":\"25.34899\",\"%wpcf-location%\":\"\\u039b\\u03b9\\u03bc\\u03ac\\u03bd\\u03b9 \\u0392\\u03bf\\u03c1\\u03bf\\u03c3\\u03ba\\u03cc\\u03c0\\u03bf\\u03c5\",\"%_wpgmp_metabox_latitude%\":\"39.854896914322005\",\"%_wpgmp_metabox_longitude%\":\"25.34899999734496\",\"%_wpgmp_location_address%\":\"V83X+XH \\u039c\\u03bf\\u03cd\\u03b4\\u03c1\\u03bf\\u03c2, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"%_wpgmp_location_city%\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"5\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/tectonic.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%wpcf-code%\":\"\",\"%_wpml_location_migration_done%\":\"1\",\"%_wpml_word_count%\":\"{\\\"total\\\":155,\\\"to_translate\\\":{\\\"en\\\":155}}\",\"%_thumbnail_id%\":\"2738\",\"%_edit_lock%\":\"1655207084:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%81%ce%ae%ce%b3%ce%bc%ce%b1-%cf%80%ce%bf%ce%bb%ce%b9%cf%8c%cf%87%ce%bd%ce%b7%cf%82-%ce%bb%ce%b9%ce%bc%ce%ac%ce%bd%ce%b9\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/46-\\u03a0\\u03bf\\u03bb\\u03b9\\u03cc\\u03c7\\u03bd\\u03b7.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"19911\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/46-\\u03a0\\u03bf\\u03bb\\u03b9\\u03cc\\u03c7\\u03bd\\u03b7.jpg, 46-\\u03a0\\u03bf\\u03bb\\u03b9\\u03cc\\u03c7\\u03bd\\u03b7, \",\"%_et_pb_truncate_post%\":\"<p>The stratigraphic contact of two separate geological formations, particularly the upper molassic sediments of Lemnos and the pyroclastic formations of Romanos, is located north of the ancient site of Poliochni on the slopes of the scenic harbor. Clays and sandstones with interstitial cobblestones (rock with rounded pebbles within) in the lower layers, aged about 23 million years, can be found with a general dip direction to the NW under the Lower Miocene tuff.<\\\/p>\\n<p>Marine sedimentogenesis occurred between 22 and 28 million years ago, resulting in the sedimentary formations of Lemnos. 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class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-kavalaris-fault\\\/\\\">Cape Kavalaris Fault<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-kavalaris-fault\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The extension of Roussopouli fault leads to the formation of Kavalaris Cape on the east coast of Lemnos. The tectonic structure may be seen east of the church of Agia Kyriaki, where parallel ruptured surfaces define the volcanic rocks and construct the shoreline to Keros Bay. The Roussopouli Fault runs for roughly 10 km in [&hellip;]<\\\/p>\\n\",\"address\":\"Unnamed Road, \\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2 814 01, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.88921424833805\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.361424294998173\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-kavalaris-fault\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The extension of Roussopouli fault leads to the formation of Kavalaris Cape on the east coast of Lemnos. The tectonic structure may be seen east of the church of Agia Kyriaki, where parallel ruptured surfaces define the volcanic rocks and construct the shoreline to Keros Bay. The Roussopouli Fault runs for roughly 10 km in [&hellip;]<\\\/p>\\n\",\"post_content\":\"The extension of Roussopouli fault leads to the formation of Kavalaris Cape on the east coast of Lemnos.\\r\\nThe tectonic structure may be seen east of the church of Agia Kyriaki, where parallel ruptured surfaces define the volcanic rocks and construct the shoreline to Keros Bay.\\r\\n\\r\\nThe Roussopouli Fault runs for roughly 10 km in a NE-SW direction and separates the Lower Miocene pyroclastic rocks from the Oligocene sedimentary formations overlaid by recent alluvial and coastal deposits.\",\"post_title\":\"Cape Kavalaris Fault\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-kavalaris-fault\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Cape Kavalaris Fault\\\" width=\\\"300\\\" height=\\\"210\\\" 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geosites\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/tectonic_result-small.png\"},\"id\":3573,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/tectonic_result-small.png\",\"name\":\"\\u03a4\\u03b5\\u03ba\\u03c4\\u03bf\\u03bd\\u03b9\\u03ba\\u03bf\\u03af\",\"id\":\"5\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Cape Ropalo Coastal Tectonic Formations\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Cape Ropalo Coastal Tectonic Formations\\\" width=\\\"300\\\" height=\\\"210\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/9-\\u0391\\u03ba\\u03c1\\u03c9\\u03c4\\u03ae\\u03c1\\u03b9\\u03bf-\\u03a1\\u03cc\\u03c0\\u03b1\\u03bb\\u03bf-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-ropalo-coastal-tectonic-formations\\\/\\\">Cape Ropalo Coastal Tectonic Formations<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-ropalo-coastal-tectonic-formations\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The southwest end of Lemnos is defined by two capes, Tigani to the west and Ropalo to the east. The presence of geological faults that split the volcanic rocks and form the tectonic coastline terrain, determines the area\\u2019s geomorphology. The eastern edge of Cape Ropalo, in particular, is produced by a sequence of faults oriented [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.832974\",\"lng\":\"25.053158\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-ropalo-coastal-tectonic-formations\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The southwest end of Lemnos is defined by two capes, Tigani to the west and Ropalo to the east. The presence of geological faults that split the volcanic rocks and form the tectonic coastline terrain, determines the area\\u2019s geomorphology. The eastern edge of Cape Ropalo, in particular, is produced by a sequence of faults oriented [&hellip;]<\\\/p>\\n\",\"post_content\":\"The southwest end of Lemnos is defined by two capes, Tigani to the west and Ropalo to the east. The presence of geological faults that split the volcanic rocks and form the tectonic coastline terrain, determines the area\\u2019s geomorphology.\\r\\n\\r\\nThe eastern edge of Cape Ropalo, in particular, is produced by a sequence of faults oriented NNW-SSE, which impact the 18.2-19.3 million year old volcanic formations that define Cape Ropalo.\",\"post_title\":\"Cape Ropalo Coastal Tectonic Formations\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-ropalo-coastal-tectonic-formations\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Cape Ropalo Coastal Tectonic Formations\\\" width=\\\"300\\\" height=\\\"210\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/9-\\u0391\\u03ba\\u03c1\\u03c9\\u03c4\\u03ae\\u03c1\\u03b9\\u03bf-\\u03a1\\u03cc\\u03c0\\u03b1\\u03bb\\u03bf-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.832974\",\"%wpcf-longtitude%\":\"25.053158\",\"%wpcf-location%\":\"\\u0391\\u03ba\\u03c1\\u03c9\\u03c4\\u03ae\\u03c1\\u03b9 \\u03a1\\u03cc\\u03c0\\u03b1\\u03bb\\u03bf\",\"%_wpgmp_metabox_latitude%\":\"39.832974\",\"%_wpgmp_metabox_longitude%\":\"25.053158\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"5\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/tectonic.png\",\"%wpcf-code%\":\"\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%_wpml_location_migration_done%\":\"1\",\"%_wpml_word_count%\":\"{\\\"total\\\":81,\\\"to_translate\\\":{\\\"en\\\":81}}\",\"%_thumbnail_id%\":\"2756\",\"%_edit_lock%\":\"1655207391:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%81%ce%b7%ce%be%ce%b9%ce%b3%ce%b5%ce%bd%ce%ae%cf%82-%ce%b1%ce%ba%cf%84%ce%ae-%ce%b1%ce%ba%cf%81%cf%89%cf%84%ce%ae%cf%81%ce%b9%ce%bf-%cf%81%cf%8c%cf%80%ce%b1%ce%bb%ce%bf\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/9-\\u0391\\u03ba\\u03c1\\u03c9\\u03c4\\u03ae\\u03c1\\u03b9\\u03bf-\\u03a1\\u03cc\\u03c0\\u03b1\\u03bb\\u03bf.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"19983\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/9-\\u0391\\u03ba\\u03c1\\u03c9\\u03c4\\u03ae\\u03c1\\u03b9\\u03bf-\\u03a1\\u03cc\\u03c0\\u03b1\\u03bb\\u03bf.jpg, 9-\\u0391\\u03ba\\u03c1\\u03c9\\u03c4\\u03ae\\u03c1\\u03b9\\u03bf \\u03a1\\u03cc\\u03c0\\u03b1\\u03bb\\u03bf, \",\"%_et_pb_truncate_post%\":\"<p>The southwest end of Lemnos is defined by two capes, Tigani to the west and Ropalo to the east. 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An impressive geological structure in the coastal zone impacts the area\\u2019s molassic formations. A system of normal faults cuts the geological formations almost entirely along the [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.80671\",\"lng\":\"25.362923\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-st-sozon-fault-formations\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Huge alternations between geological formations of sandstone and clay layers, typical of Lemnos\\u2019 molassic deposits, appear near the church of Agios Sozontas in the southeastern end of the island. An impressive geological structure in the coastal zone impacts the area\\u2019s molassic formations. A system of normal faults cuts the geological formations almost entirely along the [&hellip;]<\\\/p>\\n\",\"post_content\":\"Huge alternations between geological formations of sandstone and clay layers, typical of Lemnos\\u2019 molassic deposits, appear near the church of Agios Sozontas in the southeastern end of the island.\\r\\n\\r\\nAn impressive geological structure in the coastal zone impacts the area\\u2019s molassic formations. A system of normal faults cuts the geological formations almost entirely along the length of the beach, causing significant deformation and movement of the geological layers along the faulting planes.\",\"post_title\":\"Cape St. Sozon Fault Formations\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/cape-st-sozon-fault-formations\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Cape St. Sozon Fault Formations\\\" width=\\\"300\\\" height=\\\"209\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/48-\\u0386\\u03b3\\u03b9\\u03bf\\u03c2-\\u03a3\\u03ce\\u03b6\\u03c9\\u03bd-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" 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The existence of faults system in sedimentary rocks dating back 34-37 million years (Eocene \\u2013 Oligocene) and, more particularly, the alternations of sandstones and clays in which layers of tuffites appear, characterize the region. Opposite the church [&hellip;]<\\\/p>\\n\",\"post_content\":\"The peninsula of St. Sotira is located at the northeastern end of Lemnos, west of the Plaka peninsula. The existence of faults system in sedimentary rocks dating back 34-37 million years (Eocene \\u2013 Oligocene) and, more particularly, the alternations of sandstones and clays in which layers of tuffites appear, characterize the region.\\r\\n\\r\\nOpposite the church of Agia Sotira along the coastal slope, the layers exhibit an impressive curve which are interrupted by repeated regular fractures that form a distinctive image.\\r\\n\\r\\nNorth of the church of Agia Sotira, at the end of the road, is the scenic harbor which is part of the ruins of the old port. 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geosites\"},\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/tectonic_result-small.png\"},\"id\":3578,\"infowindow_disable\":false,\"categories\":[{\"icon\":\"\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/tectonic_result-small.png\",\"name\":\"\\u03a4\\u03b5\\u03ba\\u03c4\\u03bf\\u03bd\\u03b9\\u03ba\\u03bf\\u03af\",\"id\":\"5\",\"type\":\"category\"}]},{\"source\":\"post\",\"title\":\"Roussopouli Fault\",\"infowindow_content\":\"<div class=\\\"fc-item-box fc-item-no-padding \\\">\\r\\n    <div class=\\\"fc-feature-img\\\"><img alt=\\\"Roussopouli Fault\\\" width=\\\"300\\\" height=\\\"193\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/43-\\u03c1\\u03b7\\u03b3\\u03bc\\u03b1-\\u03c1\\u03bf\\u03c5\\u03c3\\u03c3\\u03bf\\u03c0\\u03bf\\u03c5\\u03bb\\u03b9-scaled-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\\r\\n    <div class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/roussopouli-fault\\\/\\\">Roussopouli Fault<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/roussopouli-fault\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The Roussopouli fault is a large tectonic structure about 10 km long that runs ENE-WSW and connects two different geological formations. The pyroclastic rocks are around 23 million years old (Lower Miocene), while the sedimentary rocks are approximately 33 million years old (Upper Eocene \\u2013 Lower Oligocene). The tectonic structure generates an extended terrace on [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.879009\",\"lng\":\"25.30808\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/roussopouli-fault\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The Roussopouli fault is a large tectonic structure about 10 km long that runs ENE-WSW and connects two different geological formations. The pyroclastic rocks are around 23 million years old (Lower Miocene), while the sedimentary rocks are approximately 33 million years old (Upper Eocene \\u2013 Lower Oligocene). The tectonic structure generates an extended terrace on [&hellip;]<\\\/p>\\n\",\"post_content\":\"The Roussopouli fault is a large tectonic structure about 10 km long that runs ENE-WSW and connects two different geological formations. The pyroclastic rocks are around 23 million years old (Lower Miocene), while the sedimentary rocks are approximately 33 million years old (Upper Eocene \\u2013 Lower Oligocene).\\r\\n\\r\\nThe tectonic structure generates an extended terrace on the area\\u2019s gentle landscape. It begins at Cape Sagrada, south of the village of Moudros, continues near to the settlement of Roussopouli, and terminates at Cape Kavalaris, in the harbor of Keros.\",\"post_title\":\"Roussopouli Fault\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/roussopouli-fault\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Roussopouli Fault\\\" width=\\\"300\\\" height=\\\"193\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/43-\\u03c1\\u03b7\\u03b3\\u03bc\\u03b1-\\u03c1\\u03bf\\u03c5\\u03c3\\u03c3\\u03bf\\u03c0\\u03bf\\u03c5\\u03bb\\u03b9-scaled-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.879009\",\"%wpcf-longtitude%\":\"25.30808\",\"%_wpgmp_metabox_latitude%\":\"39.879009\",\"%_wpgmp_metabox_longitude%\":\"25.30808\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"5\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/tectonic.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%wpcf-location%\":\"\",\"%wpcf-code%\":\"\",\"%_wpml_location_migration_done%\":\"1\",\"%_wpml_word_count%\":\"{\\\"total\\\":96,\\\"to_translate\\\":{\\\"en\\\":96}}\",\"%_thumbnail_id%\":\"2998\",\"%_edit_lock%\":\"1655209909:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%cf%81%ce%ae%ce%b3%ce%bc%ce%b1-%cf%81%ce%bf%cf%85%cf%83%cf%83%ce%bf%cf%80%ce%bf%cf%85%ce%bb%ce%af%ce%bf%cf%85\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/43-\\u03c1\\u03b7\\u03b3\\u03bc\\u03b1-\\u03c1\\u03bf\\u03c5\\u03c3\\u03c3\\u03bf\\u03c0\\u03bf\\u03c5\\u03bb\\u03b9.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"20097\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/43-\\u03c1\\u03b7\\u03b3\\u03bc\\u03b1-\\u03c1\\u03bf\\u03c5\\u03c3\\u03c3\\u03bf\\u03c0\\u03bf\\u03c5\\u03bb\\u03b9-scaled.jpg, 43-\\u03c1\\u03b7\\u03b3\\u03bc\\u03b1 \\u03c1\\u03bf\\u03c5\\u03c3\\u03c3\\u03bf\\u03c0\\u03bf\\u03c5\\u03bb\\u03b9, \",\"%_et_pb_truncate_post%\":\"<p>The Roussopouli fault is a large tectonic structure about 10 km long that runs ENE-WSW and connects two different geological formations. The pyroclastic rocks are around 23 million years old (Lower Miocene), while the sedimentary rocks are approximately 33 million years old (Upper Eocene \\u2013 Lower Oligocene).<\\\/p>\\n<p>The tectonic structure generates an extended terrace on the area\\u2019s gentle landscape. 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fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/pachymnos-fault\\\/\\\">Pachymnos Fault<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/pachymnos-fault\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The Pachymnos fault located towards the southeastern end of Lemnos, a few kilometers from Thanos settlement. West of the road can be seen the fault surface that forms an impressive steep slope extending to the sea. Faults are geological structures formed when tensions inside the Earth\\u2019s crust overpass the limits of rock strength, forcing it [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.845290\",\"lng\":\"25.057745\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/pachymnos-fault\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The Pachymnos fault located towards the southeastern end of Lemnos, a few kilometers from Thanos settlement. West of the road can be seen the fault surface that forms an impressive steep slope extending to the sea. Faults are geological structures formed when tensions inside the Earth\\u2019s crust overpass the limits of rock strength, forcing it [&hellip;]<\\\/p>\\n\",\"post_content\":\"The Pachymnos fault located towards the southeastern end of Lemnos, a few kilometers from Thanos settlement. West of the road can be seen the fault surface that forms an impressive steep slope extending to the sea.\\r\\n\\r\\nFaults are geological structures formed when tensions inside the Earth\\u2019s crust overpass the limits of rock strength, forcing it to break.\\r\\n\\r\\nThe nearly vertical and smooth surface is the tectonic surface of the fault, created by recent seismic activity in the area which caused the volcanic rocks to break. On this surface, the traces of rock movement emerge as slip lines (scratches). 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href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/geosites\/geomorfology\/\"><span style=\"color: #ffffff;\">Weathering-Erosion Geosites<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/geosites\/geoapotheseis\/\"><span style=\"color: #ffffff;\">Deposit Geoforms<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/geosites\/anthropogeneis\/\"><span style=\"color: #ffffff;\">Man-made Sites<\/span><\/a><\/li>\n<\/ul>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8221;1_4&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; global_colors_info=&#8221;{}&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_text ul_type=&#8221;square&#8221; _builder_version=&#8221;4.11.4&#8243; text_font=&#8221;||||||||&#8221; text_text_color=&#8221;#FFFFFF&#8221; link_font=&#8221;||||||||&#8221; link_text_color=&#8221;#ffba5a&#8221; ul_font=&#8221;||||||||&#8221; quote_font=&#8221;||||||||&#8221; 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