{"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 Geoarkeologi Peradaban Cincin Api - Departemen Teknik Geofisika","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"rnU2aiD4Qf\"><a href=\"https:\/\/www.its.ac.id\/tgeofisika\/webinar-geoarkeologi-peradaban-cincin-api-2\/\">WEBINAR Geoarkeologi Peradaban Cincin Api<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/www.its.ac.id\/tgeofisika\/webinar-geoarkeologi-peradaban-cincin-api-2\/embed\/#?secret=rnU2aiD4Qf\" width=\"600\" height=\"338\" title=\"&#8220;WEBINAR Geoarkeologi Peradaban Cincin Api&#8221; &#8212; Departemen Teknik Geofisika\" data-secret=\"rnU2aiD4Qf\" 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\/2024\/11\/Poster-Webinar-Teknik-Geofisika-ITS-Geoarkeologi-Peradaban-Cincin-Api.jpeg","thumbnail_width":1080,"thumbnail_height":1350,"description":"Nusantara terletak di jalur Ring of Fire atau cincin api Pasifik, yaitu jalur di sepanjang samudra Pasifik yang ditandai oleh gunung berapi aktif dan gempa megathrust. Ada sekitar 500 gunungapi yang tersebar di Indonesia, sekitar 129 termasuk aktif. Salah satu tanda gunungapi aktif adalah seringnya terjadi erupsi. Erupsi adalah peristiwa keluarnya magma di permukaan bumi [&hellip;]"}