{"version":"1.0","provider_name":"Geography and Natural Resources","provider_url":"https:\/\/journal.geonatres.az\/en","author_name":"Sarkhan Jafarov","author_url":"https:\/\/journal.geonatres.az\/en\/author\/emil\/","title":"MORPHOMETRIC INTERPRETATION RELIEF OF TALISH GEOSYSTEM\u00a0\u00a0 - Geography and Natural Resources","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"FtPMh3CKXV\"><a href=\"https:\/\/journal.geonatres.az\/en\/talis-geosistemi-relyefinin-morfometrik-interpretasiyasi\/\">MORPHOMETRIC INTERPRETATION RELIEF OF TALISH GEOSYSTEM\u00a0\u00a0<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/journal.geonatres.az\/en\/talis-geosistemi-relyefinin-morfometrik-interpretasiyasi\/embed\/#?secret=FtPMh3CKXV\" width=\"600\" height=\"338\" title=\"&#8220;MORPHOMETRIC INTERPRETATION RELIEF OF TALISH GEOSYSTEM\u00a0\u00a0&#8221; &#8212; Geography and Natural Resources\" data-secret=\"FtPMh3CKXV\" 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","description":"M.F.Umudova Abstract. The article discusses the methodology of horizontal and vertical (surface and deep) fragmentation maps calculated on the basis of 1: 200,000 scale to\u00adpo\u00adgraphic maps of Talysh geomorphological field, cal\u00adculated by area method, from their harmonization, the distribution of interpolation areas overlapping appro\u00adpriate values, the need to move from quantitative to qu\u00adalitative indicators, the [&hellip;]","thumbnail_url":"https:\/\/journal.geonatres.az\/wp-content\/uploads\/2026\/03\/ChatGPT-Image-27-\u043c\u0430\u0440.-2026-\u0433.-01_39_18.png","thumbnail_width":1536,"thumbnail_height":1024}