{"version":"1.0","provider_name":"Geoparco Alpi Carniche","provider_url":"https:\/\/www.geoparcoalpicarniche.org\/en\/","author_name":"Daniela De Prato","author_url":"https:\/\/www.geoparcoalpicarniche.org\/en\/author\/daniela\/","title":"The Hercynian Discord on Monte Zoufplan - Geoparco Alpi Carniche","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"behrDWJssR\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/en\/geostop\/the-hercynian-discord-on-monte-zoufplan\/\">The Hercynian Discord on Monte Zoufplan<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/www.geoparcoalpicarniche.org\/en\/geostop\/the-hercynian-discord-on-monte-zoufplan\/embed\/#?secret=behrDWJssR\" width=\"600\" height=\"338\" title=\"&#8220;The Hercynian Discord on Monte Zoufplan&#8221; &#8212; Geoparco Alpi Carniche\" data-secret=\"behrDWJssR\" frameborder=\"0\" marginwidth=\"0\" marginheight=\"0\" scrolling=\"no\" class=\"wp-embedded-content\"><\/iframe><script>\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<\/script>\n","thumbnail_url":"https:\/\/www.geoparcoalpicarniche.org\/wp-content\/uploads\/2019\/05\/93-Zoufplan-Discordanza-sotto-slargo-13_web.jpg","thumbnail_width":1204,"thumbnail_height":800,"description":"Near the summit of Pizzo del Corvo, the plane of contact between the Val Gardena Sandstone Formation (the Upper Permian) and the underlying Dimon Formation (the Lower Carboniferous) is visible. This area is recognized as a geosite of national interest. With their characteristic reddish colour, here the pelites overlap, in &hellip;"}