{"version":"1.0","provider_name":"Geography and Natural Resources","provider_url":"https:\/\/journal.geonatres.az\/en","author_name":"admin","author_url":"https:\/\/journal.geonatres.az\/en\/author\/admin\/","title":"INFLUENCE OF THE RELIEF FACTOR ON THE ECOGEOMORPHOLOGICAL CONDITIONS OF THE TALYSH MOUNTAIN REGION - Geography and Natural Resources","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"BBsnBfP3lk\"><a href=\"https:\/\/journal.geonatres.az\/en\/meqale-3\/\">INFLUENCE OF THE RELIEF FACTOR ON THE ECOGEOMORPHOLOGICAL CONDITIONS OF THE TALYSH MOUNTAIN REGION<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/journal.geonatres.az\/en\/meqale-3\/embed\/#?secret=BBsnBfP3lk\" width=\"600\" height=\"338\" title=\"&#8220;INFLUENCE OF THE RELIEF FACTOR ON THE ECOGEOMORPHOLOGICAL CONDITIONS OF THE TALYSH MOUNTAIN REGION&#8221; &#8212; Geography and Natural Resources\" data-secret=\"BBsnBfP3lk\" 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:\/\/journal.geonatres.az\/wp-includes\/js\/wp-embed.min.js\n<\/script>\n","thumbnail_url":"https:\/\/journal.geonatres.az\/wp-content\/uploads\/2019\/03\/JUrnal2019-740x1024.jpg","thumbnail_width":740,"thumbnail_height":1024,"description":"H.A.Khalilov, M.G.Almammadli mesudaz@mail.ru Abstract.\u00a0As in all mountain geomorphic systems of the Earth in the formation of ecogeomorphological conditions of the Talysh mountain region, a significant role is played by the relief, which in the complex of natural and an\u00adthropogenic factors constitutes the main component. At the same time, each of the relief factors and the [&hellip;]"}