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Using a wider definition, the Yunnan–Guizhou Highlands make up the light green area on the lower part of this map. The Yunnan–Guizhou Plateau or Yungui Plateau (simplified Chinese: 云贵高原; traditional Chinese: 雲貴高原; pinyin: Yúnguì Gāoyuán) is a highland region located in southwest China.
The Qinling and Dabashan ranges form a major north-south divide across China Proper, the traditional core area of China. Southeast of the Tibetan Plateau and south of the Sichuan Basin is the Yunnan-Guizhou Plateau, which occupies much of southwest China. This plateau, with an average elevation of 2,000 m, is known for its limestone karst ...
The Hengduan Mountains (simplified Chinese: 横断山脉; traditional Chinese: 橫斷山脈; pinyin: Héngduàn Shānmài) are a group of mountain ranges in southwest China that connect the southeast portions of the Tibetan Plateau with the Yunnan–Guizhou Plateau.
The Loess Plateau is a plateau in north-central China formed of loess, a clastic silt-like sediment formed by the accumulation of wind-blown dust. It is located southeast of the Gobi Desert and is surrounded by the Yellow River. It includes parts of the Chinese provinces of Qinghai, Gansu, Shaanxi and Shanxi. [4]
Plateaus in China develop in areas where hard rock lies above horizontal levels of rock. Most of the plateaus China are the huge area to the north and west of China Proper and range from 1,000 to 5,000 meters above sea level.
Doklam (Tibetan: འབྲོག་ལམ, Wylie: ‘brog lam, THL: drok lam), [1] [a] called Donglang (Chinese: 洞朗) by China, [5] [6] is an area in Chumbi Valley with a high plateau and a valley, lying between China's Yadong County to the north, Bhutan's Ha District to the east and India's Sikkim state to the west.
The Tibetan Plateau, [a] also known as Qinghai–Tibet Plateau [b] and Qing–Zang Plateau, [c] is a vast elevated plateau located at the intersection of South, Central, and East Asia. [d] Geographically, it is located to the north of Himalayas and the Indian subcontinent, and to the south of Tarim Basin and Mongolian Plateau.
The Yangtze plate, also called the South China block or the South China subplate, comprises the bulk of southern China.It is separated on the east from the Okinawa plate by a rift that forms the Okinawa Trough which is a back-arc basin, on the south by the Sunda plate and the Philippine Sea plate, and on the north and west by the Eurasian plate.