{"id":4231,"date":"2024-12-16T12:07:16","date_gmt":"2024-12-16T10:07:16","guid":{"rendered":"https:\/\/geopark.serverhub.gr\/item\/koziakas-thrust\/"},"modified":"2025-06-26T16:04:24","modified_gmt":"2025-06-26T13:04:24","slug":"koziakas-thrust","status":"publish","type":"citadela-item","link":"https:\/\/www.meteorapyligeopark.gr\/en\/item\/koziakas-thrust\/","title":{"rendered":"08.Koziakas Thrust"},"content":{"rendered":"<p>The Koziakas geotectonic unit, together with ophiolitic rocks, are tectonically placed towards the West on the Tertiary flysch of the Pindos belt, with a characteristic surface of compressional movement, creating the Koziakas thrust. The Koziakas tectonic thrust is indicative of the direction of compression during the final stage of the Alpine orogenesis and emergence of the Greek mountain ranges. In the eastern part of the Koziakas mountain range, the thrust of ophiolitic mixtures and a large mass of ophiolitic rocks originating from the SubPelagonic Zone, which is located a little further east, is observed in places on the rocks of the Koziakas tectonic unit.  <\/p>\n<p>Koziakas Thrust extends over a length of &gt;30 km from Diava in the north to the Portaikos valley in the south. In the southern part, the thrust becomes double, with the Koziakas formations being placed on the Thimiama Unit, which in turn is placed on the Pindos Flysch. Appearances of the Koziakas Thrust surface can be observed at various points in the Koziakas, such as along the road that crosses the Portaikos valley, on the paths leading to Koziakas from Elati and Pertouli, and further north near Diava, Krya Vrysi and Glykomilia. A very characteristic slip surface of more than 60 m in height can be seen near the village of Kotroni, along the dirt road leading south of the village. This almost vertical surface appears smooth and with friction lines, as a result of tectonic movement on the thrust. The Koziakas Thrust continues south, outside the geopark, on the southern slopes of Mount Itamos and towards Mouzaki.     <\/p>\n\r\n        <div \r\n            class=\"wp-block-citadela-blocks ctdl-item-gallery grid-type-1 layout-default size-small image-size-citadela_item_thumbnail image-vertical-align-top image-position-center-center default-image-height\"\r\n                        \t\r\n                        >\r\n            \r\n            \r\n            \r\n            <div class=\"citadela-block-articles \">\r\n               \r\n                <div class=\"citadela-block-articles-wrap citadelaFancyboxGallery \">\r\n\r\n                                            <article class=\"citadela-directory-gallery-item has-caption\">\r\n                            <div class=\"item-content\" style=\"\">\r\n                                <div class=\"item-thumbnail\">\r\n                                    <a href=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/Koziakas_Profile-scaled.jpg\" class=\"citadelaFancyboxElement\" data-gallery=\"item-gallery\" data-image-size=\"2560x1032\">\r\n                                        <img loading=\"lazy\" decoding=\"async\" \r\n                                            class=\"item-image\"\r\n                                            src=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/Koziakas_Profile-640x480.jpg\"\r\n                                            width=\"640\"\r\n                                            height=\"480\"\r\n                                            srcset=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/Koziakas_Profile-640x480.jpg 640w, https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/Koziakas_Profile-480x360.jpg 480w\"\r\n                                            sizes=\"auto, (max-width: 640px) 100vw, 640px\"\r\n                                                                                            alt=\"Simpified geological profile across Koziakas Mountain.\"\r\n                                                                                        style=\"\"                                        \/>\r\n                                                                            <\/a>\r\n                                <\/div>\r\n                            <\/div>\r\n                        <\/article>\r\n                        \r\n                                            <article class=\"citadela-directory-gallery-item has-caption\">\r\n                            <div class=\"item-content\" style=\"\">\r\n                                <div class=\"item-thumbnail\">\r\n                                    <a href=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/KoziakasThrustMap-scaled.jpg\" class=\"citadelaFancyboxElement\" data-gallery=\"item-gallery\" data-image-size=\"879x2560\">\r\n                                        <img loading=\"lazy\" decoding=\"async\" \r\n                                            class=\"item-image\"\r\n                                            src=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/KoziakasThrustMap-640x480.jpg\"\r\n                                            width=\"640\"\r\n                                            height=\"480\"\r\n                                            srcset=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/KoziakasThrustMap-640x480.jpg 640w, https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/KoziakasThrustMap-480x360.jpg 480w\"\r\n                                            sizes=\"auto, (max-width: 640px) 100vw, 640px\"\r\n                                                                                            alt=\"Map of the Koziakas Thrust with the geological formations of Koziakas Mountain.\"\r\n                                                                                        style=\"\"                                        \/>\r\n                                                                            <\/a>\r\n                                <\/div>\r\n                            <\/div>\r\n                        <\/article>\r\n                        \r\n                                            <article class=\"citadela-directory-gallery-item has-caption\">\r\n                            <div class=\"item-content\" style=\"\">\r\n                                <div class=\"item-thumbnail\">\r\n                                    <a href=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/NorthKoziakas-scaled.jpg\" class=\"citadelaFancyboxElement\" data-gallery=\"item-gallery\" data-image-size=\"2560x979\">\r\n                                        <img loading=\"lazy\" decoding=\"async\" \r\n                                            class=\"item-image\"\r\n                                            src=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/NorthKoziakas-640x480.jpg\"\r\n                                            width=\"640\"\r\n                                            height=\"480\"\r\n                                            srcset=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/NorthKoziakas-640x480.jpg 640w, https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/NorthKoziakas-480x360.jpg 480w\"\r\n                                            sizes=\"auto, (max-width: 640px) 100vw, 640px\"\r\n                                                                                            alt=\"Koziakas thrust overview along the western slope of the northern section.\"\r\n                                                                                        style=\"\"                                        \/>\r\n                                                                            <\/a>\r\n                                <\/div>\r\n                            <\/div>\r\n                        <\/article>\r\n                        \r\n                                            <article class=\"citadela-directory-gallery-item has-caption\">\r\n                            <div class=\"item-content\" style=\"\">\r\n                                <div class=\"item-thumbnail\">\r\n                                    <a href=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/DJI_0048-scaled.jpg\" class=\"citadelaFancyboxElement\" data-gallery=\"item-gallery\" data-image-size=\"2560x1263\">\r\n                                        <img loading=\"lazy\" decoding=\"async\" \r\n                                            class=\"item-image\"\r\n                                            src=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/DJI_0048-640x480.jpg\"\r\n                                            width=\"640\"\r\n                                            height=\"480\"\r\n                                            srcset=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/DJI_0048-640x480.jpg 640w, https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/DJI_0048-480x360.jpg 480w\"\r\n                                            sizes=\"auto, (max-width: 640px) 100vw, 640px\"\r\n                                                                                            alt=\"Almost vertical slip surface ~60 m high of the Koziakas Thrust, south of Kotroni. The thrust passes along the base of the slope and extends to the south towards Portaikos valley.\"\r\n                                                                                        style=\"\"                                        \/>\r\n                                                                            <\/a>\r\n                                <\/div>\r\n                            <\/div>\r\n                        <\/article>\r\n                        \r\n                                            <article class=\"citadela-directory-gallery-item has-caption\">\r\n                            <div class=\"item-content\" style=\"\">\r\n                                <div class=\"item-thumbnail\">\r\n                                    <a href=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/DJI_0006-scaled.jpg\" class=\"citadelaFancyboxElement\" data-gallery=\"item-gallery\" data-image-size=\"2560x1043\">\r\n                                        <img loading=\"lazy\" decoding=\"async\" \r\n                                            class=\"item-image\"\r\n                                            src=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/DJI_0006-640x480.jpg\"\r\n                                            width=\"640\"\r\n                                            height=\"480\"\r\n                                            srcset=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/DJI_0006-640x480.jpg 640w, https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/DJI_0006-480x360.jpg 480w\"\r\n                                            sizes=\"auto, (max-width: 640px) 100vw, 640px\"\r\n                                                                                            alt=\"The Koziakas Thrust passes almost through the middle of the image, parallel to the slope. View from the Elati-Pyli road.\"\r\n                                                                                        style=\"\"                                        \/>\r\n                                                                            <\/a>\r\n                                <\/div>\r\n                            <\/div>\r\n                        <\/article>\r\n                        \r\n                                            <article class=\"citadela-directory-gallery-item has-caption\">\r\n                            <div class=\"item-content\" style=\"\">\r\n                                <div class=\"item-thumbnail\">\r\n                                    <a href=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/DJI_0062_3_4_5_6_Enhancer_stitch-scaled.jpg\" class=\"citadelaFancyboxElement\" data-gallery=\"item-gallery\" data-image-size=\"2560x990\">\r\n                                        <img loading=\"lazy\" decoding=\"async\" \r\n                                            class=\"item-image\"\r\n                                            src=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/DJI_0062_3_4_5_6_Enhancer_stitch-640x480.jpg\"\r\n                                            width=\"640\"\r\n                                            height=\"480\"\r\n                                            srcset=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/DJI_0062_3_4_5_6_Enhancer_stitch-640x480.jpg 640w, https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/DJI_0062_3_4_5_6_Enhancer_stitch-480x360.jpg 480w\"\r\n                                            sizes=\"auto, (max-width: 640px) 100vw, 640px\"\r\n                                                                                            alt=\"Almost vertical slip surface ~60 m high of the Koziakas Thrust, south of Kotroni. The thrust passes along the base of the slope and extends to the south towards Portaikos valley.\"\r\n                                                                                        style=\"\"                                        \/>\r\n                                                                            <\/a>\r\n                                <\/div>\r\n                            <\/div>\r\n                        <\/article>\r\n                        \r\n                                    <\/div>\r\n                \r\n                \r\n            <\/div>\r\n            \r\n                        \r\n        <\/div>\r\n        ","protected":false},"excerpt":{"rendered":"<p>The Koziakas geotectonic unit, together with ophiolitic rocks, are tectonically placed towards the West on the Tertiary flysch of the Pindos belt, with a characteristic surface of compressional movement, creating the Koziakas thrust. The Koziakas tectonic thrust is indicative of the direction of compression during the final stage of the Alpine orogenesis and emergence of [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":5214,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_citadela_hide_page_title":"","_citadela_remove_header_space":"","_citadela_custom_class":"","_citadela_ignore_special_page":false,"_citadela_page_template":"","_citadela_half_map_provider":"","_citadela_half_map_theme":"","_citadela_half_map_themeOSM":"","_citadela_half_map_customTheme":"","_citadela_half_map_dataType":"","_citadela_half_map_dynamicTrack":false,"_citadela_half_map_trackColor":"","_citadela_half_map_trackEndpointsColor":"","_citadela_half_map_filterCategory":"","_citadela_half_map_filterLocation":"","_citadela_half_map_filterFeatured":false,"_citadela_half_map_noDataBehavior":"empty-map","_citadela_half_map_noDataText":"","_citadela_half_map_clusterGridSize":80,"_citadela_header":false,"_citadela_header_over_content":false,"_citadela_header_text_color":"","_citadela_header_logo":[],"_citadela_header_bg_image":[],"_citadela_header_bg_position":[],"_citadela_header_bg_size":"","_citadela_header_bg_repeat":"","_citadela_header_bg_fixed":false,"_citadela_header_bg_color":"","_citadela_header_bg_image_overlay":"","_citadela_header_transparent_bg":false,"_citadela_content_width":"","_citadela_half_layout_position":""},"citadela-item-category":[117],"citadela-item-location":[118],"class_list":["post-4231","citadela-item","type-citadela-item","status-publish","has-post-thumbnail","hentry","citadela-item-category-geological-geosites","citadela-item-location-koziakas-en"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.5 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>08.Koziakas Thrust - Meteora - Pyli Geopark<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/www.meteorapyligeopark.gr\/en\/item\/koziakas-thrust\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"08.Koziakas Thrust - Meteora - Pyli Geopark\" \/>\n<meta property=\"og:description\" content=\"The Koziakas geotectonic unit, together with ophiolitic rocks, are tectonically placed towards the West on the Tertiary flysch of the Pindos belt, with a characteristic surface of compressional movement, creating the Koziakas thrust. The Koziakas tectonic thrust is indicative of the direction of compression during the final stage of the Alpine orogenesis and emergence of [&hellip;]\" \/>\n<meta property=\"og:url\" content=\"https:\/\/www.meteorapyligeopark.gr\/en\/item\/koziakas-thrust\/\" \/>\n<meta property=\"og:site_name\" content=\"Meteora - Pyli Geopark\" \/>\n<meta property=\"article:publisher\" content=\"https:\/\/www.facebook.com\/people\/---Meteora-Pyli-Geopark\/100092757861585\/\" \/>\n<meta property=\"article:modified_time\" content=\"2025-06-26T13:04:24+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/DJI_0048-scaled.jpg\" \/>\n\t<meta property=\"og:image:width\" content=\"2560\" \/>\n\t<meta property=\"og:image:height\" content=\"1263\" \/>\n\t<meta property=\"og:image:type\" content=\"image\/jpeg\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:label1\" content=\"Est. reading time\" \/>\n\t<meta name=\"twitter:data1\" content=\"1 minute\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\\\/\\\/schema.org\",\"@graph\":[{\"@type\":\"WebPage\",\"@id\":\"https:\\\/\\\/www.meteorapyligeopark.gr\\\/en\\\/item\\\/koziakas-thrust\\\/\",\"url\":\"https:\\\/\\\/www.meteorapyligeopark.gr\\\/en\\\/item\\\/koziakas-thrust\\\/\",\"name\":\"08.Koziakas Thrust - 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