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The Gobi Desert (Mongolian: Говь, ᠭᠣᠪᠢ, / ˈ ɡ oʊ b i /; Chinese: 戈壁; pinyin: gēbì) is a large, cold desert and grassland region located in northern China and southern Mongolia. It is the sixth largest desert in the world .
The plateau includes the Gobi Desert as well as dry steppe regions. It has an elevation of roughly 1,000 to 1,500 meters (3,300 to 4,900 ft), with the lowest point in Hulunbuir and the highest point in the Altai. [1] Politically, the plateau spans all of Mongolia, along with parts of China and Russia.
However, the loess in the desert comes from the Gobi Altay Mts, the Hangayn Mts, and the Qilian Mts. The sources of loess in the Chinese Loess Plateau are the Gobi Desert and the deserts nearby, including the Tengger Desert, Badain Jaran Desert, Ulan Buh Desert, Mu Us Desert and Hobq Desert. [6] However, the main source is the Gobi Desert.
The extreme south is the Gobi Desert, some regions of which receive no precipitation at all in most years. [2] The name Gobi is a Mongol word meaning desert, depression, salt marsh, or steppe, but which usually refers to a category of arid rangeland with insufficient vegetation to support marmots but with enough to support camels. [2]
The Mongolian-Manchurian grassland (Chinese: 蒙古高原草原-内蒙古草原-东北草原) covers an area of 887,300 square kilometers (342,600 sq mi).This temperate grasslands, savannas, and shrublands ecoregion of the Palearctic realm forms a large crescent around the Gobi Desert, extending across central and eastern Mongolia into the eastern portion of Inner Mongolia and eastern and ...
The Eastern Gobi desert steppe is a deserts and xeric shrublands ecoregion in Mongolia and northern China. It is the easternmost of the ecoregions that make up the larger Gobi Desert . It lies between the more humid Mongolian–Manchurian grassland on the north, east, and southeast, and the drier Alashan Plateau semi-desert to the west.
The Alashan Plateau semi-desert ecoregion (WWF ID: PA1302) covers the southwestern portion of the Gobi Desert where precipitation in the mountains is sufficient for a short part of the summer to support sparse plant life. The terrain is basin and range, with elevations from 1,000 to 2,500 metres (3,300 to 8,200 ft).
Far view of the Flaming Cliffs. The Flaming Cliffs site (also known as Bayanzag (Chinese: 巴彥扎格), Bain-Dzak or Bayn Dzak) [1] (Mongolian: Баянзаг rich in saxaul), with the alternative Mongolian name of Mongolian: Улаан Эрэг (red cliffs), is a region of the Gobi Desert in the Ömnögovi Province of Mongolia, in which important fossil finds have been made.