{"version":"1.0","provider_name":"Geoparco Alpi Carniche","provider_url":"https:\/\/www.geoparcoalpicarniche.org\/it\/","author_name":"Daniela De Prato","author_url":"https:\/\/www.geoparcoalpicarniche.org\/it\/author\/daniela\/","title":"Il masso erratico, regalo dell\u2019era glaciale - Geoparco Alpi Carniche","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"GUlFDGwxDC\"><a href=\"https:\/\/www.geoparcoalpicarniche.org\/it\/geostop\/masso-erratico\/\">Il masso erratico, regalo dell\u2019era glaciale<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/www.geoparcoalpicarniche.org\/it\/geostop\/masso-erratico\/embed\/#?secret=GUlFDGwxDC\" width=\"600\" height=\"338\" title=\"&#8220;Il masso erratico, regalo dell\u2019era glaciale&#8221; &#8212; Geoparco Alpi Carniche\" data-secret=\"GUlFDGwxDC\" 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\/04\/geotrail8_web.jpg","thumbnail_width":1920,"thumbnail_height":1277,"description":"Accanto al ponte, sulla sponda del torrente, si trova un grande masso laminato di colore rosso-grigio. Ad un\u2019osservazione pi\u00f9 attenta si individuano sulla sua superficie delle strutture reticolari, formate da particelle argillose scure che racchiudono nuclei calcarei pi\u00f9 chiari. Le rocce che presentano tali strutture sono denominate \u201cflaser\u201d, e la &hellip;"}