{"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":"Netzkalke \u2013 auffallende Strukturen - Geoparco Alpi Carniche","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"lzizyWDk6O\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/de\/geostop\/i-calcari-della-formazione-del-findenig\/\">Netzkalke \u2013 auffallende Strukturen<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/www.geoparcoalpicarniche.org\/de\/geostop\/i-calcari-della-formazione-del-findenig\/embed\/#?secret=lzizyWDk6O\" width=\"600\" height=\"338\" title=\"&#8220;Netzkalke \u2013 auffallende Strukturen&#8221; &#8212; Geoparco Alpi Carniche\" data-secret=\"lzizyWDk6O\" 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\/02\/HP17_DSC03474_2-1280.jpg","thumbnail_width":1280,"thumbnail_height":960,"description":"Die Netzkalke der Findenig-Formation entstanden aus einem tonreichen Kalkschlamm, der sich im Devon vor rund 390 Millionen Jahren in Meerestiefen von \u00fcber 100 Metern ablagerte. Er enth\u00e4lt vorwiegend Geh\u00e4use und Skelette von mikroskopisch kleinen Organismen (Plankton). Im Gestein wechseln sich dunkelrote, tonreiche Partien mit hellroten, kalkdominierten Partien ab. Diese spezielle &hellip;"}