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The Changjiang Plain evergreen forests ecoregion (WWF ID: PA0415) covers the plain of the Yangtze River (Changjiang) from where it leaves the mountains at the Three Gorges in the west, to the mouth of the Yangtze at the East China Sea. This plain is one of the most densely populated areas on Earth, and most of the original oak and conifer ...
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).
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 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 ...
Map of the Three Gorges After arriving at Yibin ( 宜宾 ), in Sichuan Province ( 四川 ), the Yangtze River ( 长江 ) flows from Jiangjin ( 江津 ), of Chongqing Municipality ( 重庆 ), to Yichang ( 宜昌 ), of Hubei Province ( 湖北 ); and this section of the river is called Chuanjiang ( 川江 ), or "the river of Sichuan".
It is made up of alluvial deposits from the Yangtze River and its tributaries. The plain is somewhat swampy, made up of many lakes and rivers, making it suitable for rice growing and freshwater fish, and it is therefore known as the "land of fish and rice".
Yangtze River Delta Economic Region [3]. 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 alluvial East China plain extends from just south of Beijing in the north, to the Yangtze River delta in the south, punctuated only by the igneous Shandong highlands and peninsula. [3] [5] South of the Yangtze river, most of the landscape is mountainous, dominated by sedimentary deposits and by the South China Craton.