{"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":"Panoramic view of the Cima di Lanza - Geoparco Alpi Carniche","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"QMhH9ebZVD\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/en\/geostop\/panoramic-view-of-the-cima-di-lanza\/\">Panoramic view of the Cima di Lanza<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/www.geoparcoalpicarniche.org\/en\/geostop\/panoramic-view-of-the-cima-di-lanza\/embed\/#?secret=QMhH9ebZVD\" width=\"600\" height=\"338\" title=\"&#8220;Panoramic view of the Cima di Lanza&#8221; &#8212; Geoparco Alpi Carniche\" data-secret=\"QMhH9ebZVD\" 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\/06\/Geostop09_CimadiLanza.jpg","thumbnail_width":2304,"thumbnail_height":3072,"description":"The stratified aspect of the Cima di Lanza that we can observe to the east is due to an alternation of more compact calcareous banks and less cohesive pelitic strata. These rocks were laid down between the Upper Carboniferous and Lower Permian (about 320-280 million years ago) in a period &hellip;"}