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The Yungui Plateau is a large mountainous region with rugged terrain including steep karst peaks and deep gorges. [5] The plateau is buttressed by the large Hengduan Mountains to the northwest and by lowland regions to the north, east, and southeast. Other major mountain ranges cross or surround portions of the Yungui Plateau.
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.
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.
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 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 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]
Hate it or love it, China is a global superpower, and in order to understand its complexities, one must look not just at the headlines but also at everyday life, where nuanced societal trends and ...
Shimao (Chinese: 石峁; pinyin: Shímǎo) is a Neolithic site in Shenmu County, Shaanxi, China. The site is located in the northern part of the Loess Plateau, on the southern edge of the Ordos Desert. It is dated to around 2000 BC, near the end of the Longshan period, and is the largest known walled site of that period in China, at 400 ha.