{"version":"1.0","provider_name":"Departemen Teknik Geofisika","provider_url":"https:\/\/www.its.ac.id\/tgeofisika","author_name":"Admin-Teknik Geofisika","author_url":"https:\/\/www.its.ac.id\/tgeofisika\/author\/tgeofisikaadmin\/","title":"WEBINAR #49: TERIMA KASIH GUNUNG API - Departemen Teknik Geofisika","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"eTyFQUmtea\"><a href=\"https:\/\/www.its.ac.id\/tgeofisika\/en\/webinar-49-terima-kasih-gunung-api\/\">WEBINAR #49: TERIMA KASIH GUNUNG API<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/www.its.ac.id\/tgeofisika\/en\/webinar-49-terima-kasih-gunung-api\/embed\/#?secret=eTyFQUmtea\" width=\"600\" height=\"338\" title=\"&#8220;WEBINAR #49: TERIMA KASIH GUNUNG API&#8221; &#8212; Departemen Teknik Geofisika\" data-secret=\"eTyFQUmtea\" 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.its.ac.id\/tgeofisika\/wp-includes\/js\/wp-embed.min.js\n<\/script>\n","thumbnail_url":"https:\/\/www.its.ac.id\/tgeofisika\/wp-content\/uploads\/sites\/33\/2022\/01\/Webinar-Terima-Kasih-Gunung-Api-2022.jpeg","thumbnail_width":1280,"thumbnail_height":1280,"description":"The core of the earth, like the sun, is where radioactive reactions take place and will produce hot magma and high pressure. The difference in heat will cause convection currents that move the plates away from each other, approach each other, or pass each other. Indonesia is pressed by 3 plates from the south, north [&hellip;]"}