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Map of current configuration of Yellow River system, and the Luo (Lo) River. The Yellow River (Chinese: Huang He) flows from the Tibetan Plateau to the Bay of Bohai over a course of 5,464 kilometers (3,395 mi), making it the second-longest river in Asia and the sixth-longest in the world.
The Yellow River as depicted in a Qing dynasty illustrated map (sections) Historical courses of the Yellow River Historical courses of the Yellow River. In Chinese mythology, the giant Kua Fu drained the Yellow River and the Wei River to quench his burning thirst as he pursued the Sun. [31] Historical documents from the Spring and Autumn period ...
Map of tribes and tribal unions in Ancient China. Yanhuang is shown as Hua Xia Tribal Union in the map. Yanhuang or Yan Huang (simplified Chinese: 炎 黄; traditional Chinese: 炎 黃; pinyin: Yán Huáng) was the name of a mythical ethnic group of ancient China who were said to have inhabited the Yellow River basin area.
The part of the North China Plain around the banks of the middle and lower Yellow River is commonly referred to as the Central Plain (pinyin: Zhōngyuán). This portion of the North China Plain formed the cradle of Chinese civilization, and is the region from which the Han Chinese people emerged. [1] [2]
When the Yellow River approaches the Hukou Mountain, blocked by mountains on both sides, its width is abruptly narrowed down to 20–30 m (66–98 ft). The water's velocity increases, and then plunges over a narrow opening on a cliff, forming a waterfall 15 m (49 ft) high and 20 m (66 ft) wide, as if water were pouring down from a huge teapot.
Provincial boundaries. The Loess Plateau is shaded. The Yellow River is colored blue. The yellow area is Inner Mongolia and Ningxia. The Ordos Plateau, also known as the Ordos Basin or simply the Ordos, is a highland sedimentary basin in parts of most Northern China with an elevation of 1,000–1,600 m (3,300–5,200 ft), and consisting mostly of land enclosed by the Ordos Loop, a large ...
The Yellow River carries more sediment than any other in the world. [ 1 ] [ 2 ] During the 18 months after the river was closed, 1.8 billion metric tons of sediment had accumulated in the reservoir. Only 7% of the sediment-load was released downstream and the reservoir lost 17% of its capacity below a 335 m (1,099 ft) ASL elevation.
The mountains mark the divide between the drainage basins of the Yangtze and Yellow River systems, providing a natural boundary between North and South China and support a huge variety of plant and wildlife, some of which is found nowhere else on earth. To the north is the densely populated Wei River valley, an ancient center of Chinese ...