Prehistoric Mongolia
id:
prehistoric-mongolia-166-14368712
title:
Prehistoric Mongolia
text:
The climate of Central Asia became dry after the large tectonic collision between the Indian Plate and the Eurasian Plate. This impact threw up the massive chain of mountains known as the Himalayas. The Himalayas, Greater Khingan and Lesser Khingan mountains act like a high wall, blocking the warm and wet climate from penetrating into Central Asia. Many of the mountains of Mongolia were formed during the Late Neogene and Early Quaternary periods. The Mongolian climate was more humid hundreds of
brand slug:
wiki
category slug:
encyclopedia
description:
Events in Mongolia before Antiquity
original url:
https://en.wikipedia.org/wiki/Prehistoric_Mongolia
date created:
2013-07-30T11:07:40Z
date modified:
2024-08-30T12:35:29Z
main entity:
{"identifier":"Q17053048","url":"https://www.wikidata.org/entity/Q17053048"}
image:
fields total:
13
integrity:
15