{"version":"1.0","provider_name":"Geoparco Alpi Carniche","provider_url":"https:\/\/www.geoparcoalpicarniche.org\/de\/","author_name":"omnia","author_url":"https:\/\/www.geoparcoalpicarniche.org\/de\/author\/omnia\/","title":"Das K\u00e4nozoikum und die alpidische Orogenese - Geoparco Alpi Carniche","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"e9nqOlTEBD\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/de\/ere_geologiche\/era-cenozoica-e-orogenesi-alpina\/\">Das K\u00e4nozoikum und die alpidische Orogenese<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/www.geoparcoalpicarniche.org\/de\/ere_geologiche\/era-cenozoica-e-orogenesi-alpina\/embed\/#?secret=e9nqOlTEBD\" width=\"600\" height=\"338\" title=\"&#8220;Das K\u00e4nozoikum und die alpidische Orogenese&#8221; &#8212; Geoparco Alpi Carniche\" data-secret=\"e9nqOlTEBD\" 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\/2018\/03\/7.cenozoico_neoz_wu\u0308rm.jpg","thumbnail_width":1420,"thumbnail_height":680,"description":"Am Beginn des K\u00e4nozoikums, (vor 65 Millionen Jahren) nach dem Verschwinden der Dinosaurier und Ammoniten, ist Karnien von einem warmen seichten Meer bedeckt. In dieser Umgebung lagern sich Kalksedimente ab, die reich an kleinen M\u00fcnzen f\u00f6rmigen Schalentierchen sind, den Nummuliten (aus. Lat. nummus: M\u00fcnze)."}