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The Changjiang Water Resources Commission (CWRC; [1] simplified Chinese: 长江水利委员会; traditional Chinese: 長江水利委員會; pinyin: Chángjiāng shuǐlì wěiyuánhuì) is a river basin authority dispatched by the Ministry of Water Resources of the People's Republic of China to exercise water administrative functions in the Yangtze River Basin and other river basins of ...
The Yangtze River Plain stretches 1,000 km from the Three Gorges to the sea. The terrain is mostly flat or low alluvial hills, with numerous shallow lakes. Large lakes include Poyang Lake , the largest freshwater lake in China, and Dongting Lake which was formerly the largest but has seen significant conversion to farmland over the years.
The "Great River" with its entrance to the East China Sea marked as the "Mouth of the Yangtze" (揚子 江口) on the Jiangnan map in the 1754 Provincial Atlas of the Qing Empire. By the Han dynasty, Jiāng had come to mean any river in Chinese, and this river was distinguished as the "Great River" 大江 (Dàjiāng).
The Yangtze (Chang Jiang) rises in Tibet, flows through Central China and enters the East China Sea near Shanghai. The Yangtze is 6,300 kilometers long and has a catchment area of 1.8 million square kilometers. It is the third longest river in the world, after the Amazon and the Nile. The second longest river in China is the Huang He (Yellow ...
Yangtze River (Chang Jiang 长江; upper reach known as Jinsha Jiang 金沙江 and Tongtian River 通天河) (For detailed list see List of tributaries of the Yangtze.) Huangpu River (黃浦江) Suzhou Creek or Wusong River (苏州河, 吴淞江) Xitiao River (西苕溪) Daxi Creek; Grand Canal (大运河) Qinhuai River. Gaoyou Lake (高邮湖)
The Changhua River (Chinese: 昌化江), [4] also known as Changhua Jiang, [5] Chang River (昌江), [6] is a river located in Hainan Province of the People's Republic of China. [ 7 ] and is the second longest river in Hainan .
The Yangtze Delta or Yangtze River Delta (YRD, Chinese: 长江三角洲 or simply 长三角), once known as the Shanghai Economic Zone, is a megalopolis generally comprising the Wu-speaking areas of Shanghai, southern Jiangsu, northern Zhejiang, southern Anhui.
The geology of China (or the geological structure of the People's Republic of China) consists of three Precambrian cratons surrounded by a number of orogenic belts. The modern tectonic environment is dominated by the continued collision of India with the rest of Asia starting 40–50 million years ago.