Traditional Culture Encyclopedia - The 24 Solar Terms - What is the soil type of Qinghai-Tibet Plateau?
What is the soil type of Qinghai-Tibet Plateau?
The soil types of Qinghai-Tibet Plateau are alpine meadow soil, subalpine meadow soil, alpine grassland soil, mountain meadow soil, subalpine steppe soil and meadow soil.
Qinghai-Tibet Plateau is the largest plateau in China and the highest plateau in the world. Known as the "roof of the world" and "roof of the world". It starts from the southern edge of Himalayas in the south, reaches Kunlun Mountain, Altun Mountain and the northern edge of Qilian Mountain in the north, reaches Pamir Plateau and Karakorum Mountain in the west, and borders western Qinling Mountain and Loess Plateau in the east and northeast.
The Qinghai-Tibet Plateau is about 2,800 kilometers long from east to west and 300 ~ 1.500 kilometers wide from north to south, with a total area of about 2.5 million square kilometers. Topographically, it can be divided into six parts: Northern Tibet Plateau, Southern Tibet Valley, Qaidam Basin, Qilian Mountain, Qinghai Plateau and Sichuan-Tibet Alpine Canyon, including all Tibet in China and parts of Qinghai, Xinjiang, Gansu, Sichuan and Yunnan, as well as Bhutan, Nepal and India.
The natural and historical development of the Qinghai-Tibet Plateau is extremely young. Influenced by many factors, it has formed the highest and youngest natural geographical unit in the world, with a close combination of horizontal zonality and vertical zonality. The annual average temperature in the hinterland of the plateau is below 0℃, and the monthly average temperature in the warmest area is also below 10℃. The Qinghai-Tibet Plateau is generally between 3000 and 5000 meters above sea level, with an average elevation of more than 4000 meters. It is the birthplace of many rivers in East Asia, Southeast Asia and South Asia. There are many lakes on the plateau, including Namtso and Qinghai Lake.
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