1.0Meteora - Pyli Geoparkhttps://www.meteorapyligeopark.gr/en/adminhttps://www.meteorapyligeopark.gr/en/author/support_2oe85v0r/rich600338<blockquote class="wp-embedded-content" data-secret="pGbC0fbKbb"><a href="https://www.meteorapyligeopark.gr/en/item/gavros-landforms/">04.Gavros Landforms</a></blockquote><iframe sandbox="allow-scripts" security="restricted" src="https://www.meteorapyligeopark.gr/en/item/gavros-landforms/embed/#?secret=pGbC0fbKbb" width="600" height="338" title="“04.Gavros Landforms” — Meteora - Pyli Geopark" data-secret="pGbC0fbKbb" frameborder="0" marginwidth="0" marginheight="0" scrolling="no" class="wp-embedded-content"></iframe><script> /*! This file is auto-generated */ !function(d,l){"use strict";l.querySelector&&d.addEventListener&&"undefined"!=typeof URL&&(d.wp=d.wp||{},d.wp.receiveEmbedMessage||(d.wp.receiveEmbedMessage=function(e){var t=e.data;if((t||t.secret||t.message||t.value)&&!/[^a-zA-Z0-9]/.test(t.secret)){for(var s,r,n,a=l.querySelectorAll('iframe[data-secret="'+t.secret+'"]'),o=l.querySelectorAll('blockquote[data-secret="'+t.secret+'"]'),c=new RegExp("^https?:$","i"),i=0;i<o.length;i++)o[i].style.display="none";for(i=0;i<a.length;i++)s=a[i],e.source===s.contentWindow&&(s.removeAttribute("style"),"height"===t.message?(1e3<(r=parseInt(t.value,10))?r=1e3:~~r<200&&(r=200),s.height=r):"link"===t.message&&(r=new URL(s.getAttribute("src")),n=new URL(t.value),c.test(n.protocol))&&n.host===r.host&&l.activeElement===s&&(d.top.location.href=t.value))}},d.addEventListener("message",d.wp.receiveEmbedMessage,!1),l.addEventListener("DOMContentLoaded",function(){for(var e,t,s=l.querySelectorAll("iframe.wp-embedded-content"),r=0;r<s.length;r++)(t=(e=s[r]).getAttribute("data-secret"))||(t=Math.random().toString(36).substring(2,12),e.src+="#?secret="+t,e.setAttribute("data-secret",t)),e.contentWindow.postMessage({message:"ready",secret:t},"*")},!1)))}(window,document); //# sourceURL=https://www.meteorapyligeopark.gr/wp-includes/js/wp-embed.min.js </script> https://www.meteorapyligeopark.gr/wp-content/uploads/2024/12/Gavros_rocks-scaled.jpg25601920The landforms of Gavros are a continuation of the Meteora complex to the north. The rocky outcrops of cohesive conglomerates and sandstones of the Meteora Conglomerate unit were deposited as submarine drifts and belong to the Meso-Hellenic Trench, as part of the Pentalophos-Meteora Formation of Upper Oligocene – Lower Miocene age (10-30 million years). The […]