{"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":"Pal\u00e4ozoikum: Karbon - Geoparco Alpi Carniche","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"0U6BrKX8dB\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/de\/ere_geologiche\/carbonifero\/\">Pal\u00e4ozoikum: Karbon<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/www.geoparcoalpicarniche.org\/de\/ere_geologiche\/carbonifero\/embed\/#?secret=0U6BrKX8dB\" width=\"600\" height=\"338\" title=\"&#8220;Pal\u00e4ozoikum: Karbon&#8221; &#8212; Geoparco Alpi Carniche\" data-secret=\"0U6BrKX8dB\" 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\/2018\/03\/4.carbonifero_illustraz.jpg","thumbnail_width":1420,"thumbnail_height":680,"description":"W\u00e4hrend des Karbons (von vor 360 bis 300 Millionen Jahren) lagerten sich insbesondere Sand und Silikat Schlammaus der Erosion der Urgebirge ab. Dazu kamen unter Wasser Vulkanit Schichten, durch vereinzelte vulkanische Erscheinungen."}