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</html><thumbnail_url>https://www.meteorapyligeopark.gr/wp-content/uploads/2024/12/DJI_0048-scaled.jpg</thumbnail_url><thumbnail_width>2560</thumbnail_width><thumbnail_height>1263</thumbnail_height><description>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;]</description></oembed>
