{"version":"1.0","provider_name":"Geoparco Alpi Carniche","provider_url":"https:\/\/www.geoparcoalpicarniche.org\/de\/","author_name":"Daniela De Prato","author_url":"https:\/\/www.geoparcoalpicarniche.org\/de\/author\/daniela\/","title":"Kleine Klamm des Rio Bordaglia - Geoparco Alpi Carniche","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"GvHc71aZIG\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/de\/geostop\/kleine-klamm-des-rio-bordaglia\/\">Kleine Klamm des Rio Bordaglia<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/www.geoparcoalpicarniche.org\/de\/geostop\/kleine-klamm-des-rio-bordaglia\/embed\/#?secret=GvHc71aZIG\" width=\"600\" height=\"338\" title=\"&#8220;Kleine Klamm des Rio Bordaglia&#8221; &#8212; Geoparco Alpi Carniche\" data-secret=\"GvHc71aZIG\" 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\/07\/01_Forra-rio-Bordaglia.jpg","thumbnail_width":2100,"thumbnail_height":2800,"description":"Der Rio Bordaglia hat in seiner letzten Strecke eine kleine Klamm ausgeh\u00f6hlt. Die Erosion, die den Flusslauf vertieft hat, hat kompakte Marmorsteine getroffen, die aus verwandelten devonischen Kalksteinen stammen. An diesem Punkt kann man einige Morphologien beobachten, die diese Umgebungen charakterisieren, wie Erosionst\u00f6pfe und vom Wasser gegl\u00e4ttete Felsen."}