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Eastern Gobi desert steppe, the easternmost of the Gobi ecoregions, covering an area of 281,800 km 2 (108,804 sq mi). It extends from the Inner Mongolian Plateau in China northward into Mongolia. It includes the Yin Mountains and many low-lying areas with salt pans and small ponds.
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 Gobi Lakes Valley is about 500 km (310 mi) west-to-east, and 150 km (93 mi) north-to south, at elevations of 1,000–1,400 metres (3,300–4,600 ft). [2] The region is desert steppe, with rivers from the Khangai Mountains on the north providing most of the water to the lakes. On the south the region is bounded by the Gobi-Altai range, the ...
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).
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. [1]
Map of the Palearctic realm Subcategories. This category has the following 41 subcategories, out of 41 total. ... Gobi Desert (45 P) I. ... Sahara desert (ecoregion ...
The Altai-Sayan ecoregion is located at the intersection of the Central Asian and Siberian faunal provinces. The Altai mountains are home to a diverse fauna, because of its different habitats, like steppes, northern taigas and alpine vegetation.
Generally evaporation exceeds rainfall in these ecoregions. Temperature variability is also diverse in these lands. Many deserts, such as the Sahara, are hot year-round, but others, such as East Asia's Gobi Desert, become quite cold during the winter. [1] Temperature extremes are a characteristic of most deserts.