{"id":4243,"date":"2024-12-16T11:53:08","date_gmt":"2024-12-16T09:53:08","guid":{"rendered":"https:\/\/geopark.serverhub.gr\/item\/panagia-ophiolites\/"},"modified":"2025-06-26T16:03:29","modified_gmt":"2025-06-26T13:03:29","slug":"panagia-ophiolites","status":"publish","type":"citadela-item","link":"https:\/\/www.meteorapyligeopark.gr\/en\/item\/panagia-ophiolites\/","title":{"rendered":"14.Panagia Ophiolites"},"content":{"rendered":"<p>The ophiolite outcrops around the village of Panagia are among the most interesting outcrops of the ophiolite sequence of the Pindos Mountain range. The Pindos ophiolites represent parts of the Tethys oceanic lithosphere that were emplaced over the Pindos flysch during the Tertiary. The ophiolitic rocks of Pindus include basic and ultrabasic igneous rocks (upper mantle peridotites, gabbros, basic and ultrabasic igneous rocks, columnar lavas, massive lavas, pillow lavas, and basic breccias), metamorphic rocks derived from the metamorphic sole (amphibolites, greenschists, and meta-sediments) as well as deep-sea sediments and turbidites (pelagic limestones, sandstones, calcareous sandstones, and microbreccias, mudstones, green and red bedded and nodular radiolarites).  <\/p>\n<p>The various rocks and formations encountered in the wider area of \u200b\u200bPanagia are mapped as a series of different units, part of the Pindus Ophiolitic Complex. These units (Avdella, Aspropotamos, Dramala) are placed as tectonic plates on the Pindus flysch. The Avdella unit (Avdella m\u00e9lange) consists of a diverse mixture (m\u00e9lange) of various volcanic, sedimentary rocks as well as blocks of surrounding formations. This mixture was created as a result of tectonic deformation and mild metamorphism at the base of the Ophiolite complex. The volcanic rocks of the ophiolites were formed in Mid-Ocean ridge conditions, in an ocean east of the Pindus Zone. A corresponding current environment is the emergence of lava and formation of oceanic crust in the center of the Atlantic Ocean. Intense tectonic flaking and deformation has led to the local fragmentation of the various formations and the presence of fault structures that can be seen along the road. The age of the rocks of these formations is mainly Jurassic, with a range ranging from Triassic to Upper Cretaceous.       <\/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\/Profile_Jones_1991-1.png\" class=\"citadelaFancyboxElement\" data-gallery=\"item-gallery\" data-image-size=\"3493x1357\">\r\n                                        <img loading=\"lazy\" decoding=\"async\" \r\n                                            class=\"item-image\"\r\n                                            src=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/Profile_Jones_1991-1-640x480.png\"\r\n                                            width=\"640\"\r\n                                            height=\"480\"\r\n                                            srcset=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/Profile_Jones_1991-1-640x480.png 640w, https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/Profile_Jones_1991-1-480x360.png 480w\"\r\n                                            sizes=\"auto, (max-width: 640px) 100vw, 640px\"\r\n                                                                                            alt=\"Schematic geological section showing the emplacement of the Ophiolitic Complex units.\"\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\/PANO_20250210_162725-scaled.jpg\" class=\"citadelaFancyboxElement\" data-gallery=\"item-gallery\" data-image-size=\"2560x1061\">\r\n                                        <img loading=\"lazy\" decoding=\"async\" \r\n                                            class=\"item-image\"\r\n                                            src=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/PANO_20250210_162725-640x480.jpg\"\r\n                                            width=\"640\"\r\n                                            height=\"480\"\r\n                                            srcset=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/PANO_20250210_162725-640x480.jpg 640w, https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/PANO_20250210_162725-480x360.jpg 480w\"\r\n                                            sizes=\"auto, (max-width: 640px) 100vw, 640px\"\r\n                                                                                            alt=\"Ultramafic rock outcrop along the Panagia-Koridallos 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\/PANO_20250210_162038.jpg\" class=\"citadelaFancyboxElement\" data-gallery=\"item-gallery\" data-image-size=\"2382x1200\">\r\n                                        <img loading=\"lazy\" decoding=\"async\" \r\n                                            class=\"item-image\"\r\n                                            src=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/PANO_20250210_162038-640x480.jpg\"\r\n                                            width=\"640\"\r\n                                            height=\"480\"\r\n                                            srcset=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/PANO_20250210_162038-640x480.jpg 640w, https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/PANO_20250210_162038-480x360.jpg 480w\"\r\n                                            sizes=\"auto, (max-width: 640px) 100vw, 640px\"\r\n                                                                                            alt=\"Outcrop of strongly tectonically deformed ultramafic rocks along the main road, north of Panagia.\"\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\/Panagia_rocks-topaz.jpg\" class=\"citadelaFancyboxElement\" data-gallery=\"item-gallery\" data-image-size=\"1537x1618\">\r\n                                        <img loading=\"lazy\" decoding=\"async\" \r\n                                            class=\"item-image\"\r\n                                            src=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/Panagia_rocks-topaz-640x480.jpg\"\r\n                                            width=\"640\"\r\n                                            height=\"480\"\r\n                                            srcset=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/Panagia_rocks-topaz-640x480.jpg 640w, https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/Panagia_rocks-topaz-480x360.jpg 480w\"\r\n                                            sizes=\"auto, (max-width: 640px) 100vw, 640px\"\r\n                                                                                            alt=\"Basalt lavas in the Panagia area.\"\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\/Panagia_II-topaz.jpg\" class=\"citadelaFancyboxElement\" data-gallery=\"item-gallery\" data-image-size=\"2472x1738\">\r\n                                        <img loading=\"lazy\" decoding=\"async\" \r\n                                            class=\"item-image\"\r\n                                            src=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/Panagia_II-topaz-640x480.jpg\"\r\n                                            width=\"640\"\r\n                                            height=\"480\"\r\n                                            srcset=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/Panagia_II-topaz-640x480.jpg 640w, https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/Panagia_II-topaz-480x360.jpg 480w\"\r\n                                            sizes=\"auto, (max-width: 640px) 100vw, 640px\"\r\n                                                                                            alt=\"Oceanic sediments (clay shales), strongly tectonized and folded, near Panagia. They are part of the volcanosedimentary series of the ophiolite complex.\"\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 ophiolite outcrops around the village of Panagia are among the most interesting outcrops of the ophiolite sequence of the Pindos Mountain range. The Pindos ophiolites represent parts of the Tethys oceanic lithosphere that were emplaced over the Pindos flysch during the Tertiary. The ophiolitic rocks of Pindus include basic and ultrabasic igneous rocks (upper [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":5303,"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":[85],"class_list":["post-4243","citadela-item","type-citadela-item","status-publish","has-post-thumbnail","hentry","citadela-item-category-geological-geosites","citadela-item-location-kalambaka-en"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.6 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>14.Panagia Ophiolites - 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\/panagia-ophiolites\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"14.Panagia Ophiolites - Meteora - Pyli Geopark\" \/>\n<meta property=\"og:description\" content=\"The ophiolite outcrops around the village of Panagia are among the most interesting outcrops of the ophiolite sequence of the Pindos Mountain range. The Pindos ophiolites represent parts of the Tethys oceanic lithosphere that were emplaced over the Pindos flysch during the Tertiary. The ophiolitic rocks of Pindus include basic and ultrabasic igneous rocks (upper [&hellip;]\" \/>\n<meta property=\"og:url\" content=\"https:\/\/www.meteorapyligeopark.gr\/en\/item\/panagia-ophiolites\/\" \/>\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=\"2025-06-26T13:03:29+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/www.meteorapyligeopark.gr\/wp-content\/uploads\/2024\/12\/PANO_20250210_162725-scaled.jpg\" \/>\n\t<meta property=\"og:image:width\" content=\"2560\" \/>\n\t<meta property=\"og:image:height\" content=\"1061\" \/>\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\\\/panagia-ophiolites\\\/\",\"url\":\"https:\\\/\\\/www.meteorapyligeopark.gr\\\/en\\\/item\\\/panagia-ophiolites\\\/\",\"name\":\"14.Panagia Ophiolites - 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