{"version":"1.0","provider_name":"Geoparco Alpi Carniche","provider_url":"https:\/\/www.geoparcoalpicarniche.org\/de\/","author_name":"Daniela De Prato","author_url":"https:\/\/www.geoparcoalpicarniche.org\/de\/author\/daniela\/","title":"Wolayer Kopf, Hohe Warte und Creta di Chianevate - Geoparco Alpi Carniche","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"E5yey2p9dn\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/de\/geostop\/wolayer-kopf-hohe-warte-und-creta-di-chianevate\/\">Wolayer Kopf, Hohe Warte und Creta di Chianevate<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/www.geoparcoalpicarniche.org\/de\/geostop\/wolayer-kopf-hohe-warte-und-creta-di-chianevate\/embed\/#?secret=E5yey2p9dn\" width=\"600\" height=\"338\" title=\"&#8220;Wolayer Kopf, Hohe Warte und Creta di Chianevate&#8221; &#8212; Geoparco Alpi Carniche\" data-secret=\"E5yey2p9dn\" frameborder=\"0\" marginwidth=\"0\" marginheight=\"0\" scrolling=\"no\" class=\"wp-embedded-content\"><\/iframe><script type=\"text\/javascript\">\n\/* <![CDATA[ *\/\n\/*! This file is auto-generated *\/\n!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);\n\/\/# sourceURL=https:\/\/www.geoparcoalpicarniche.org\/wp-includes\/js\/wp-embed.min.js\n\/* ]]> *\/\n<\/script>\n","thumbnail_url":"https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2019\/07\/05_Monte-Volaia-da-Passo-Giramondo.jpg","thumbnail_width":3008,"thumbnail_height":2000,"description":"Von diesem Punkt aus bietet sich Richtung Osten ein Panoramablick auf den Wolayer Kopf, die Hohe Warte und Creta di Chianevate. Diese Reliefs bestehen aus Plattformkalksteinen aus dem Devon (vor 420 bis 360 Millionen Jahren) und bilden den Kern der imposantesten, pal\u00e4ozoischen, organogenen Klippe, die heute in Europa sichtbar ist. &hellip;"}