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	{"id":3257,"date":"2021-06-30T11:40:50","date_gmt":"2021-06-30T08:40:50","guid":{"rendered":"https:\/\/www.lemnosgeomonuments.gr\/geosites\/volcanos\/"},"modified":"2022-03-24T15:58:58","modified_gmt":"2022-03-24T13:58:58","slug":"volcanos","status":"publish","type":"page","link":"https:\/\/www.lemnosgeomonuments.gr\/en\/geosites\/volcanos\/","title":{"rendered":"Volcanic geosites"},"content":{"rendered":"<p>[et_pb_section fb_built=&#8221;1&#8243; admin_label=&#8221;Header&#8221; _builder_version=&#8221;4.11.4&#8243; use_background_color_gradient=&#8221;on&#8221; background_color_gradient_start=&#8221;rgba(165,206,199,0.6)&#8221; background_color_gradient_end=&#8221;#151f33&#8243; background_color_gradient_overlays_image=&#8221;on&#8221; background_image=&#8221;https:\/\/www.lemnosgeomonuments.gr\/wp-content\/uploads\/2022\/01\/10-\u0397\u03c6\u03b1\u03b9\u03c3\u03c4\u03b5\u03b9\u03b1\u03ba\u03cc\u03c2-\u03b4\u03cc\u03bc\u03bf\u03c2-\u0391\u03b3\u03af\u03bf\u03c5-\u03a0\u03b1\u03cd\u03bb\u03bf\u03c5-scaled.jpg&#8221; 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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>Volcanic Geosites<br \/><\/strong><\/p>\n<p>Approximately 23 million years ago, Greece\u2019s volcanic activity was mainly located in the region of the North Aegean. During that period, important volcanic centers were active in Lemnos.<\/p>\n<p>In eastern Lemnos, visitors can see the legacy of this volcanic activity during the Lower Miocene -approximately 23 million years ago. Large volcanic domes, volcanic dykes, large pyroclastic flows, as well as hot springs, help the visitors begin to understand the enormity and reality of these once active volcanoes. They can examine the impressive volcanic structures up close and enjoy walking along the trails which wind between the 23-million-year-old volcanoes.<\/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 orderby=&#8221;rand&#8221; custom_post_types=&#8221;simeio&#8221; include_categories=&#8221;2&#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; 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 map<\/h3>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column 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The volcanic dome on the hill of Saint Pavlos is a conical volcanic formation composed of dacitic lava which formed 19.3-18.2 million years ago. The formation of this dome is related to the intense volcanic activity that created [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.845\",\"lng\":\"25.104\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/st-pavlos-volcanic-dome\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Near the town of Thanos in SW Lemnos, a highly distinctive volcanic formation stands by the sea. The volcanic dome on the hill of Saint Pavlos is a conical volcanic formation composed of dacitic lava which formed 19.3-18.2 million years ago. The formation of this dome is related to the intense volcanic activity that created [&hellip;]<\\\/p>\\n\",\"post_content\":\"Near the town of Thanos in SW Lemnos, a highly distinctive volcanic formation stands by the sea. The volcanic dome on the hill of Saint Pavlos is a conical volcanic formation composed of dacitic lava which formed 19.3-18.2 million years ago.\\r\\n\\r\\nThe formation of this dome is related to the intense volcanic activity that created the chain of volcanic domes in southwestern Lemnos. Rising magma with a high potassium and silicon concentration permeated the pre-existing sedimentary and pyroclastic geological formations, causing their uplifting. 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The volcanic dome on the hill of Saint Pavlos is a conical volcanic formation composed of dacitic lava which formed 19.3-18.2 million years ago.<\\\/p>\\n<p>The formation of this dome is related to the intense volcanic activity that created the chain of volcanic domes in southwestern Lemnos. Rising magma with a high potassium and silicon concentration permeated the pre-existing sedimentary and pyroclastic geological formations, causing their uplifting. 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This characteristic volcanic structure is a set of parallel and nearly vertical lava \\u201cwalls\\u201d that stand upright in the surrounding plain. This volcanic structure was formed by the intrusion of andesitic magma through faults in the crust where it [&hellip;]<\\\/p>\\n\",\"address\":\"V4F2+CV \\u039c\\u03cd\\u03c1\\u03b9\\u03bd\\u03b1, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.87360108165118\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.102158714294447\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kakavos-volcanic-dyke\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The Kakavos Volcanic dyke is located alongside the road that leads to the Kakavos volcanic hill. This characteristic volcanic structure is a set of parallel and nearly vertical lava \\u201cwalls\\u201d that stand upright in the surrounding plain. This volcanic structure was formed by the intrusion of andesitic magma through faults in the crust where it [&hellip;]<\\\/p>\\n\",\"post_content\":\"The Kakavos Volcanic dyke is located alongside the road that leads to the Kakavos volcanic hill. This characteristic volcanic structure is a set of parallel and nearly vertical lava \\u201cwalls\\u201d that stand upright in the surrounding plain.\\r\\n\\r\\nThis volcanic structure was formed by the intrusion of andesitic magma through faults in the crust where it solidified with time, creating the impressive volcanic structure. 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class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/profitis-ilias-volcanic-dome\\\/\\\">Profitis Ilias Volcanic Dome<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/profitis-ilias-volcanic-dome\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The impressive hill of Profitis Ilias dominating the landscape is one of the most characteristic volcanic structures of Lemnos. Located to the west of the gulf of Moudros, south of the village of Kornos, the hot springs of Therma flow from its foothills. The volcanic dome was formed by the uplifting of the volcanic rocks [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.896\",\"lng\":\"25.129\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/profitis-ilias-volcanic-dome\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The impressive hill of Profitis Ilias dominating the landscape is one of the most characteristic volcanic structures of Lemnos. Located to the west of the gulf of Moudros, south of the village of Kornos, the hot springs of Therma flow from its foothills. The volcanic dome was formed by the uplifting of the volcanic rocks [&hellip;]<\\\/p>\\n\",\"post_content\":\"The impressive hill of Profitis Ilias dominating the landscape is one of the most characteristic volcanic structures of Lemnos. Located to the west of the gulf of Moudros, south of the village of Kornos, the hot springs of Therma flow from its foothills.\\r\\n\\r\\nThe volcanic dome was formed by the uplifting of the volcanic rocks as dacitic lava permeated the crust. The hill of Profitis Ilias belongs to a complex of volcanic structures created 19.3-18.2 million years ago in western Lemnos by magma with a relatively high gas content which permeated and uplifted pre-existing geological formations before it rapidly cooled.\\r\\n\\r\\nAt the highest points of the volcanic dome there are weathering formations called \\u201ctafoni\\u201d, which are fascinating structures caused by erosion of the volcanic rocks.\\r\\n\\r\\nThe towering volcanic hill of Profitis Ilias appears to have been well-known among foreign visitors. There are instances, such as that of the French Ambassador to the Ottoman Empire, Auguste de Choiseul \\u2013 Gouffie (1785), where the volcanic structure is referred to as the Therma Mountain (Mt. de Therma).\",\"post_title\":\"Profitis Ilias Volcanic Dome\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/profitis-ilias-volcanic-dome\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Profitis Ilias Volcanic Dome\\\" width=\\\"300\\\" height=\\\"215\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/19-\\u03a0\\u03c1\\u03bf\\u03c6\\u03ae\\u03c4\\u03b7\\u03c2-\\u0397\\u03bb\\u03af\\u03b1\\u03c2-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.896\",\"%wpcf-longtitude%\":\"25.129\",\"%wpcf-location%\":\"\\u03a0\\u03c1\\u03bf\\u03c6\\u03ae\\u03c4\\u03b7\\u03c2 \\u0397\\u03bb\\u03af\\u03b1\\u03c2\",\"%_wpgmp_metabox_latitude%\":\"39.896\",\"%_wpgmp_metabox_longitude%\":\"25.129\",\"%_wpgmp_location_address%\":\"\",\"%_wpgmp_location_city%\":\"\",\"%_wpgmp_location_state%\":\"\",\"%_wpgmp_location_country%\":\"\",\"%_wpgmp_metabox_location_redirect%\":\"marker\",\"%_wpgmp_metabox_custom_link%\":\"\",\"%_wpgmp_map_id%\":\"a:2:{i:0;s:1:\\\"1\\\";i:1;s:1:\\\"2\\\";}\",\"%_wpgmp_metabox_marker_id%\":\"a:1:{i:0;s:1:\\\"4\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/volcanos.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%wpcf-code%\":\"\",\"%_wpml_location_migration_done%\":\"1\",\"%_wpml_word_count%\":\"{\\\"total\\\":181,\\\"to_translate\\\":{\\\"en\\\":181}}\",\"%_thumbnail_id%\":\"2766\",\"%_edit_lock%\":\"1655205339:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%b7%cf%86%ce%b1%ce%b9%cf%83%cf%84%ce%b5%ce%b9%ce%b1%ce%ba%cf%8c%cf%82-%ce%b4%cf%8c%ce%bc%ce%bf%cf%82-%cf%80%cf%81%ce%bf%cf%86%ce%ae%cf%84%ce%b7%cf%82-%ce%b7%ce%bb%ce%af%ce%b1%cf%82\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/19-\\u03a0\\u03c1\\u03bf\\u03c6\\u03ae\\u03c4\\u03b7\\u03c2-\\u0397\\u03bb\\u03af\\u03b1\\u03c2.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"19571\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/19-\\u03a0\\u03c1\\u03bf\\u03c6\\u03ae\\u03c4\\u03b7\\u03c2-\\u0397\\u03bb\\u03af\\u03b1\\u03c2.jpg, 19-\\u03a0\\u03c1\\u03bf\\u03c6\\u03ae\\u03c4\\u03b7\\u03c2 \\u0397\\u03bb\\u03af\\u03b1\\u03c2, \",\"%_et_pb_truncate_post%\":\"<p>The impressive hill of Profitis Ilias dominating the landscape is one of the most characteristic volcanic structures of Lemnos. Located to the west of the gulf of Moudros, south of the village of Kornos, the hot springs of Therma flow from its foothills.<\\\/p>\\n<p>The volcanic dome was formed by the uplifting of the volcanic rocks as dacitic lava permeated the crust. The hill of Profitis Ilias belongs to a complex of volcanic structures created 19.3-18.2 million years ago in western Lemnos by magma with a relatively high gas content which permeated and uplifted pre-existing geological formations before it rapidly cooled.<\\\/p>\\n<p>At the highest points of the volcanic dome there are weathering formations called \\u201ctafoni\\u201d, which are fascinating structures caused by erosion of the volcanic rocks.<\\\/p>\\n<p>The towering volcanic hill of Profitis Ilias appears to have been well-known among foreign visitors. 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from the parking lot on the road to the chapel of Panagia Kakaviotissa. The scattered hills in the area form a network of volcanic structures that were created 19.3-18.2 million years ago. The permeation of viscous magma [&hellip;]<\\\/p>\\n\",\"address\":\"V4H6+RF \\u039c\\u03cd\\u03c1\\u03b9\\u03bd\\u03b1, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.87919279928601\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.111099701019278\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/palaiokastro-volcanic-dome\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Palaiokastro Volcanic Dome is a characteristic volcanic structure in the western part of Lemnos, visible to the visitor from the parking lot on the road to the chapel of Panagia Kakaviotissa. The scattered hills in the area form a network of volcanic structures that were created 19.3-18.2 million years ago. The permeation of viscous magma [&hellip;]<\\\/p>\\n\",\"post_content\":\"Palaiokastro Volcanic Dome is a characteristic volcanic structure in the western part of Lemnos, visible to the visitor from the parking lot on the road to the chapel of Panagia Kakaviotissa.\\r\\n\\r\\nThe scattered hills in the area form a network of volcanic structures that were created 19.3-18.2 million years ago. The permeation of viscous magma with high gas content caused the uplifting of older sedimentary and volcanic rock. Erosion, in turn, revealed the solidified lava that created these characteristic domed structures.\",\"post_title\":\"Palaiokastro Volcanic Dome\",\"post_link\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/palaiokastro-volcanic-dome\\\/\",\"post_featured_image\":\"<div class=\\\"fc-feature-img\\\"><img alt=\\\"Palaiokastro Volcanic Dome\\\" width=\\\"300\\\" height=\\\"210\\\" src=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/17-\\u0397\\u03c6\\u03b1\\u03b9\\u03c3\\u03c4\\u03b5\\u03b9\\u03b1\\u03ba\\u03cc\\u03c2-\\u03b4\\u03cc\\u03bc\\u03bf\\u03c2-\\u03a0\\u03b1\\u03bb\\u03b1\\u03b9\\u03cc\\u03ba\\u03b1\\u03c3\\u03c4\\u03c1\\u03bf\\u03c5-medium.jpg\\\" class=\\\"wp-post-image   wpgmp_featured_image\\\" ><\\\/div>\",\"post_categories\":\"\",\"post_tags\":\"\",\"%_wp_page_template%\":\"default\",\"%wpcf-latitude%\":\"39.87919\",\"%wpcf-longtitude%\":\"25.11109\",\"%wpcf-location%\":\"\\u03a0\\u03b1\\u03bb\\u03b1\\u03b9\\u03cc\\u03ba\\u03b1\\u03c3\\u03c4\\u03c1\\u03bf\",\"%_wpgmp_metabox_latitude%\":\"39.87919279928601\",\"%_wpgmp_metabox_longitude%\":\"25.111099701019278\",\"%_wpgmp_location_address%\":\"V4H6+RF \\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:\\\"4\\\";}\",\"%_wpgmp_metabox_taxomomies_terms%\":\"N;\",\"%_wpgmp_extensions_fields%\":\"N;\",\"%_wpv_contains_gutenberg_views%\":\"\",\"%wpcf-mapicon%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2021\\\/07\\\/volcanos.png\",\"%_wpml_media_duplicate%\":\"1\",\"%_wpml_media_featured%\":\"1\",\"%wpcf-code%\":\"\",\"%_wpml_location_migration_done%\":\"1\",\"%_wpml_word_count%\":\"{\\\"total\\\":100,\\\"to_translate\\\":{\\\"en\\\":100}}\",\"%_thumbnail_id%\":\"2765\",\"%_edit_lock%\":\"1655205427:1\",\"%_edit_last%\":\"1\",\"%_wp_old_slug%\":\"%ce%b7%cf%86%ce%b1%ce%b9%cf%83%cf%84%ce%b5%ce%b9%ce%b1%ce%ba%cf%8c%cf%82-%ce%b4%cf%8c%ce%bc%ce%bf%cf%82-%cf%80%ce%b1%ce%bb%ce%b1%ce%b9%cf%8c%ce%ba%ce%b1%cf%83%cf%84%cf%81%ce%bf%cf%85\",\"%wpcf-image-gallery%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/17-\\u0397\\u03c6\\u03b1\\u03b9\\u03c3\\u03c4\\u03b5\\u03b9\\u03b1\\u03ba\\u03cc\\u03c2-\\u03b4\\u03cc\\u03bc\\u03bf\\u03c2-\\u03a0\\u03b1\\u03bb\\u03b1\\u03b9\\u03cc\\u03ba\\u03b1\\u03c3\\u03c4\\u03c1\\u03bf\\u03c5.jpg\",\"%_wpcf-image-gallery-sort-order%\":\"19607\",\"%_last_translation_edit_mode%\":\"native-editor\",\"%_xmlsf_image_attached%\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/wp-content\\\/uploads\\\/2020\\\/07\\\/17-\\u0397\\u03c6\\u03b1\\u03b9\\u03c3\\u03c4\\u03b5\\u03b9\\u03b1\\u03ba\\u03cc\\u03c2-\\u03b4\\u03cc\\u03bc\\u03bf\\u03c2-\\u03a0\\u03b1\\u03bb\\u03b1\\u03b9\\u03cc\\u03ba\\u03b1\\u03c3\\u03c4\\u03c1\\u03bf\\u03c5.jpg, 17-\\u0397\\u03c6\\u03b1\\u03b9\\u03c3\\u03c4\\u03b5\\u03b9\\u03b1\\u03ba\\u03cc\\u03c2 \\u03b4\\u03cc\\u03bc\\u03bf\\u03c2 \\u03a0\\u03b1\\u03bb\\u03b1\\u03b9\\u03cc\\u03ba\\u03b1\\u03c3\\u03c4\\u03c1\\u03bf\\u03c5, \",\"%_et_pb_truncate_post%\":\"<p>Palaiokastro Volcanic Dome is a characteristic volcanic structure in the western part of Lemnos, visible to the visitor from the parking lot on the road to the chapel of Panagia Kakaviotissa.<\\\/p>\\n<p>The scattered hills in the area form a network of volcanic structures that were created 19.3-18.2 million years ago. 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class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kakavos-volcanic-domes\\\/\\\">Kakavos Volcanic Domes<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kakavos-volcanic-domes\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Northeast of the village of Thanos is a chain of conical hills which are the volcanic structures that characterize the unique landscape of southwest Lemnos. These volcanic structures were formed 19.3-18.2 million years ago, when dacitic magma rose to the surface through tectonic discontinuities in the crust, permeating pre-existing sedimentary and volcanic formations. When the [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.870\",\"lng\":\"25.108\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kakavos-volcanic-domes\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Northeast of the village of Thanos is a chain of conical hills which are the volcanic structures that characterize the unique landscape of southwest Lemnos. These volcanic structures were formed 19.3-18.2 million years ago, when dacitic magma rose to the surface through tectonic discontinuities in the crust, permeating pre-existing sedimentary and volcanic formations. When the [&hellip;]<\\\/p>\\n\",\"post_content\":\"Northeast of the village of Thanos is a chain of conical hills which are the volcanic structures that characterize the unique landscape of southwest Lemnos.\\r\\n\\r\\nThese volcanic structures were formed 19.3-18.2 million years ago, when dacitic magma rose to the surface through tectonic discontinuities in the crust, permeating pre-existing sedimentary and volcanic formations. When the viscous magma surfaced, it cooled swiftly, thus forming the characteristic dome structures.\\r\\n\\r\\nThese volcacin domes show intense erosion by strong winds, resulting in the formations of \\u201ctafoni\\u201d cavities. 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fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/therma-hot-springs\\\/\\\">Therma Hot Springs<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/therma-hot-springs\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Hot springs emerging at the foot of the hill of Profitis Ilias in the Therma region have been used since ancient times. At a temperature of 42-44 degrees Celsius, the water wells up from 2 springs at a depth of around 1200 meters. The water is safe to drink and ideal for balneotherapy. The existence [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.905384\",\"lng\":\"25.122017\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/therma-hot-springs\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Hot springs emerging at the foot of the hill of Profitis Ilias in the Therma region have been used since ancient times. At a temperature of 42-44 degrees Celsius, the water wells up from 2 springs at a depth of around 1200 meters. The water is safe to drink and ideal for balneotherapy. The existence [&hellip;]<\\\/p>\\n\",\"post_content\":\"Hot springs emerging at the foot of the hill of Profitis Ilias in the Therma region have been used since ancient times. At a temperature of 42-44 degrees Celsius, the water wells up from 2 springs at a depth of around 1200 meters. The water is safe to drink and ideal for balneotherapy.\\r\\n\\r\\nThe existence of hot springs is related to the existence of geological faults and active tectonic activity today. Surface waters find a way down into the crust through the discontinuities in the rocks. There, the water meets the magmatic chambers of Lemnos\\u2019 volcanoes, which were once active 20 million years ago and are now enriched with various minerals and gases. Water returns to the surface through the faults with the help of gases and gushes up in the form of hot springs.\\r\\n\\r\\nTherma\\u2019s original thermal bath infrastructure remains intact, including a tiny changing room and a stone bathtub built in the 16th century. 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class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kodias-volcanic-dome\\\/\\\">Kodias Volcanic Dome<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kodias-volcanic-dome\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>Alongside the Myrina-Kodias road, the Kodias Volcanic Dome stands out in strong contrast to the flat surrounding landscape. The hill consists of dacitic lava which was formed 19.3-18.2 million years ago. The Kodias Volcanic Dome is a part of the wider group of volcanic structures that characterize the south-west region of Lemnos. Rising magma, rich [&hellip;]<\\\/p>\\n\",\"location\":{\"lat\":\"39.863\",\"lng\":\"25.147\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/kodias-volcanic-dome\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>Alongside the Myrina-Kodias road, the Kodias Volcanic Dome stands out in strong contrast to the flat surrounding landscape. The hill consists of dacitic lava which was formed 19.3-18.2 million years ago. The Kodias Volcanic Dome is a part of the wider group of volcanic structures that characterize the south-west region of Lemnos. 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The Kodias Volcanic Dome is a part of the wider group of volcanic structures that characterize the south-west region of Lemnos.<\\\/p>\\n<p>Rising magma, rich in gas content, moved up most likely through tectonic faults and created this structure. 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class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/evgatis-volcanic-dome\\\/\\\">Evgatis Volcanic Dome<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/evgatis-volcanic-dome\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The Evgatis Volcanic Dome is located in the southwest region of Lemnos, east of the town of Thanos. Composed of trachyandesite, the volcanic hill\\u2019s shape is characterized by steep and rugged slopes which are associated with the intense volcanic activity that caused magma to rise 19.3-18.2 million years ago. The activity that created this volcanic [&hellip;]<\\\/p>\\n\",\"address\":\"V436+XF \\u039c\\u03cd\\u03c1\\u03b9\\u03bd\\u03b1, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.854884693219134\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.111171298980718\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/evgatis-volcanic-dome\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The Evgatis Volcanic Dome is located in the southwest region of Lemnos, east of the town of Thanos. Composed of trachyandesite, the volcanic hill\\u2019s shape is characterized by steep and rugged slopes which are associated with the intense volcanic activity that caused magma to rise 19.3-18.2 million years ago. The activity that created this volcanic [&hellip;]<\\\/p>\\n\",\"post_content\":\"The Evgatis Volcanic Dome is located in the southwest region of Lemnos, east of the town of Thanos. Composed of trachyandesite, the volcanic hill\\u2019s shape is characterized by steep and rugged slopes which are associated with the intense volcanic activity that caused magma to rise 19.3-18.2 million years ago. The activity that created this volcanic dome is responsible for the formation of a series of other volcanic domes that are scattered throughout western Lemnos.\\r\\n\\r\\nDuring this period of time, viscous magma with a high content of potassium and silicon permeated into the geological formation through faults in the earth\\u2019s crust. 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Composed of trachyandesite, the volcanic hill\\u2019s shape is characterized by steep and rugged slopes which are associated with the intense volcanic activity that caused magma to rise 19.3-18.2 million years ago. The activity that created this volcanic dome is responsible for the formation of a series of other volcanic domes that are scattered throughout western Lemnos.<\\\/p>\\n<p>During this period of time, viscous magma with a high content of potassium and silicon permeated into the geological formation through faults in the earth\\u2019s crust. This resulted in the general uplifting of the area. 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class=\\\"fc-itemcontent-padding fc-text-center\\\">\\r\\n        <div class=\\\"fc-itemcontent-padding fc-item-no-padding fc-item-margin\\\">\\r\\n            <div class=\\\"fc-item-title fc-item-primary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/myrina-volcanic-dome\\\/\\\">Myrina Volcanic Dome<\\\/a><\\\/div>\\r\\n            <div class=\\\"fc-item-meta fc-item-secondary-text-color\\\"><a href=\\\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/myrina-volcanic-dome\\\/\\\">\\u0394\\u03b9\\u03b1\\u03b2\\u03ac\\u03c3\\u03c4\\u03b5 \\u03c0\\u03b5\\u03c1\\u03b9\\u03c3\\u03c3\\u03cc\\u03c4\\u03b5\\u03c1\\u03b1...<\\\/a><\\\/div>\\r\\n        <\\\/div>\\r\\n    <\\\/div>\\r\\n    <div class=\\\"fc-clear\\\"><\\\/div>\\r\\n<\\\/div>\",\"content\":\"<p>The impressive peninsula, upon which the byzantine castle of Myrina is built, lies between two sandy beaches, Roman and the Turkish Gialos. This peninsula was formed 19.3-18.2 million years ago, when the intense volcanic activity caused dacitic magma to rise and permeate the crust, where it cooled instantly, creating the steep volcanic dome that characterizes [&hellip;]<\\\/p>\\n\",\"address\":\"V3G3+RG \\u039c\\u03cd\\u03c1\\u03b9\\u03bd\\u03b1, \\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"location\":{\"lat\":\"39.877058416910906\",\"city\":\"\\u039b\\u03ae\\u03bc\\u03bd\\u03bf\\u03c2\",\"country\":\"\\u0395\\u03bb\\u03bb\\u03ac\\u03b4\\u03b1\",\"lng\":\"25.053927116394032\",\"onclick_action\":\"marker\",\"redirect_permalink\":\"https:\\\/\\\/www.lemnosgeomonuments.gr\\\/en\\\/simeio\\\/myrina-volcanic-dome\\\/\",\"zoom\":5,\"extra_fields\":{\"post_excerpt\":\"<p>The impressive peninsula, upon which the byzantine castle of Myrina is built, lies between two sandy beaches, Roman and the Turkish Gialos. This peninsula was formed 19.3-18.2 million years ago, when the intense volcanic activity caused dacitic magma to rise and permeate the crust, where it cooled instantly, creating the steep volcanic dome that characterizes [&hellip;]<\\\/p>\\n\",\"post_content\":\"The impressive peninsula, upon which the byzantine castle of Myrina is built, lies between two sandy beaches, Roman and the Turkish Gialos. This peninsula was formed 19.3-18.2 million years ago, when the intense volcanic activity caused dacitic magma to rise and permeate the crust, where it cooled instantly, creating the steep volcanic dome that characterizes the area.\\r\\n\\r\\nThe volcanic rock is porphyritic, meaning mineral crystals can be distinguished easily in the glassy mass. 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{\r\npadding:0px !important;\r\n\r\n}\r\n\r\n.wpgmp_tabs_container .wpgmp_tabs li a.active {\r\nbackground-color: #a5bab2 !important;\r\n}\r\n.wpgmp_toggle_container {display:none}\r\n.wpgmp_tabs_container {top:12% !important}\r\n.wpgmp_tabs_container {width:25% !important; right: 14px!important;}<\/style>\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;Footer&#8221; _builder_version=&#8221;4.9.7&#8243; background_color=&#8221;#00140b&#8221; custom_padding=&#8221;5px||0vw||false|&#8221; global_module=&#8221;3360&#8243; saved_tabs=&#8221;all&#8221; collapsed=&#8221;off&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_row column_structure=&#8221;1_4,1_4,1_4,1_4&#8243; _builder_version=&#8221;3.25&#8243; custom_margin=&#8221;|78px||auto||&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;1_4&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; 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global_colors_info=&#8221;{}&#8221;]<\/p>\n<p><span style=\"font-size: large;\"><strong>Geosites<\/strong><\/span><\/p>\n<ul>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/geosites\/volcanos\/\"><span style=\"color: #ffffff;\">Volcanic Geosites<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/geosites\/apolithomata\/\"><span style=\"color: #ffffff;\">Fossils<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/geosites\/tektonikoi\/\"><span style=\"color: #ffffff;\">Tectonic Geosites<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/geosites\/water\/\"><span style=\"color: #ffffff;\">Hydrographic Systems<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/geosites\/%cf%80%ce%b1%cf%81%ce%ac%ce%ba%cf%84%ce%b9%ce%b5%cf%82-%ce%b3%ce%b5%cf%89%ce%bc%ce%bf%cf%81%cf%86%ce%ad%cf%82\/\"><span style=\"color: #ffffff;\">Coastal Geosites<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/geosites\/geomorfology\/\"><span style=\"color: #ffffff;\">Weathering-Erosion Geosites<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/geosites\/geoapotheseis\/\"><span style=\"color: #ffffff;\">Deposit Geoforms<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/geosites\/anthropogeneis\/\"><span style=\"color: #ffffff;\">Man-made Sites<\/span><\/a><\/li>\n<\/ul>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8221;1_4&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; global_colors_info=&#8221;{}&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_text ul_type=&#8221;square&#8221; _builder_version=&#8221;4.11.4&#8243; text_font=&#8221;||||||||&#8221; text_text_color=&#8221;#FFFFFF&#8221; link_font=&#8221;||||||||&#8221; link_text_color=&#8221;#ffba5a&#8221; ul_font=&#8221;||||||||&#8221; quote_font=&#8221;||||||||&#8221; custom_margin=&#8221;10px|||||&#8221; locked=&#8221;off&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<p><span style=\"font-size: large;\"><strong>Culture<\/strong><\/span><\/p>\n<ul>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/culture\/ancient_sites\/\"><span style=\"color: #ffffff;\">Archaeological Sites<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/culture\/churches\/\"><span style=\"color: #ffffff;\">Religious Monuments<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/culture\/monuments\/\"><span style=\"color: #ffffff;\">Modern Monuments<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/culture\/villages\/\"><span style=\"color: #ffffff;\">Lemnos Settlements<\/span><\/a><\/li>\n<li><a href=\"https:\/\/www.lemnosgeomonuments.gr\/en\/culture\/museums\/\"><span style=\"color: #ffffff;\">Museums<\/span><\/a><\/li>\n<\/ul>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8221;1_4&#8243; 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