List of rivers of China

This incomplete list of rivers that flow through China is organized according to the body of water into which each river empties, beginning with the Sea of Okhotsk in the northeast, moving clockwise on a map and ending with the Atlantic ocean.

Sea of Okhotsk

Amur River basin

Sea of Japan

Bohai Sea

  • Anzi River (鞍子河)
  • Fuzhou River (复州河)
  • Daliao River (大辽河)
Liao River Basin
Wei River Basin
Yellow River Basin

Yellow Sea

Huai River basin

East China Sea

Han River Basin of Hubei, southern Shaanxi and southwestern Henan
Jialing River Basin of Chongqing, eastern Sichuan and southern Gansu
Min sichuan rivermap
Min River of central Sichuan
Yalong River of western Sichuan and southern Qinghai

Taiwan Strait

South China Sea

Pearl River Basin

From Hainan Island

Hainan - Haikou - Nandu rivermap
Nandu River (map), Hainan Province

Andaman Sea

  • Nu River (怒江) / (Salween River)
    • Wanma River (万马河)
    • Hongyang River (硔养河)
    • Mengboluo River (勐波罗河)
    • Supa River (苏帕河)
    • Shidian River (施甸河)
    • Luomingba River (罗明坝河)
  • Irrawaddy River (Myanmar)

Bay of Bengal

Ganges-Brahmaputra-Meghna basins
Map of the Ganges (yellow), Brahmaputra (violet), and Meghna (green) drainage basins.

Arabian Sea

Arctic Ocean

Ob watershed
Ob-Irtysh watershed
  • Ob River (Russia)
    • Irtysh (额尔齐斯河)
      • Bieliezeke River (别列则克河)
      • Haba River (哈巴河)
      • Burqin River (布尔津河)
      • Kala Irtysh River (喀拉额尔齐斯河)

Endorheic basins

Tarim Basin

Tarim Basin
Ili Basin

Dzungarian Basin

Juyan Lake Basin

Lake Balkhash

Lake Alakol


See also

External links

Brahmaputra River

The Brahmaputra () is one of the major rivers of Asia, a trans-boundary river which flows through China, India and Bangladesh. As such, it is known by various names in the region: Assamese: লুইত luit [luɪt], ব্ৰহ্মপুত্ৰ নৈ Brohmoputro noi, ব্ৰহ্মপুত্ৰ নদ (the tatsama 'নদ' nod, masculine form of the tatsama 'নদী' nodi "river") Brohmoputro [bɹɔɦmɔputɹɔ]; Sanskrit: ब्रह्मपुत्र, IAST: Brahmaputra; Tibetan: ཡར་ཀླུངས་གཙང་པོ་, Wylie: yar klung gtsang po Yarlung Tsangpo; simplified Chinese: 布拉马普特拉河; traditional Chinese: 布拉馬普特拉河; pinyin: Bùlāmǎpǔtèlā Hé. It is also called Tsangpo-Brahmaputra and red river of India (when referring to the whole river including the stretch within Tibet). The Manas River, which runs through Bhutan, joins it at Jogighopa, in India. It is the ninth largest river in the world by discharge, and the 15th longest.

With its origin in the Manasarovar Lake region, located on the northern side of the Himalayas in Burang County of Tibet as the Yarlung Tsangpo River, it flows across southern Tibet to break through the Himalayas in great gorges (including the Yarlung Tsangpo Grand Canyon) and into Arunachal Pradesh (India). It flows southwest through the Assam Valley as Brahmaputra and south through Bangladesh as the Jamuna (not to be mistaken with Yamuna of India). In the vast Ganges Delta, it merges with the Padma, the popular name of the river Ganges in Bangladesh, and finally the Meghna and from here it is known as Meghna before emptying into the Bay of Bengal.About 2,899.9 km (1,801.9 mi) long, the Brahmaputra is an important river for irrigation and transportation. The average depth of the river is 38 m (124 ft) and maximum depth is 120 m (380 ft). The river is prone to catastrophic flooding in the spring when Himalayas snow melts. The average discharge of the river is about 19,800 m3/s (700,000 cu ft/s), and floods can reach over 100,000 m3/s (3,500,000 cu ft/s). It is a classic example of a braided river and is highly susceptible to channel migration and avulsion. It is also one of the few rivers in the world that exhibit a tidal bore. It is navigable for most of its length.

The river drains the Himalaya east of the Indo-Nepal border, south-central portion of the Tibetan plateau above the Ganga basin, south-eastern portion of Tibet, the Patkai-Bum hills, the northern slopes of the Meghalaya hills, the Assam plains, and the northern portion of Bangladesh. The basin, especially south of Tibet, is characterized by high levels of rainfall. Kangchenjunga (8,586 m) is the only peak above 8,000 m, hence is the highest point within the Brahmaputra basin.

The Brahmaputra's upper course was long unknown, and its identity with the Yarlung Tsangpo was only established by exploration in 1884–86. This river is often called the Tsangpo-Brahmaputra river.

The lower reaches are sacred to Hindus. While most rivers on the Indian subcontinent have female names, this river has a rare male name, as it means "son of Brahma" in Sanskrit (putra means "son").

Fu River (Jiangxi)

The Fu River, or Fuhe (Chinese: 抚河), is a river in China's Jiangxi province. Its basin occupies most of the Fuzhou prefecture of Jiangxi.

The Fu River has it origin on the northwestern slopes of the Wuyi Mountains, from where it flows in the general north-northwestern and northwestern direction. Via a network of smaller lakes and channels in Nanchang prefecture, the waters of the Fuhe eventually reach the Poyang Lake, to which it is one of the major tributaries, along with the Gan River (which flows from the south/southwest) and a number of smaller rivers coming from the east and west.

As the Poyang Lake drains into the Yangtze, the Fu River is part of the Yangtze Basin as well.

Jin River (Fujian)

The Jin River, also known by its Chinese name Jin Jiang, is located in southern Fujian. Its basin includes most of Quanzhou prefecture-level city, whose Jinjiang County is named after it.

Keriya River

The Keriya River is a river in the province of Xinjiang in China. It flows for 519 km (322 mi) from the Kunlun Shan mountain range north into the endorheic Tarim Basin, but is lost in the desert several hundred kilometers south of the Tarim River. The only major settlement along the river is Keriya Town, east of Hotan. The river is an important source of irrigation water and also supplies historically important oases along its course. Its drainage basin covers about 7,358 km2 (2,841 sq mi).Situated in an extremely arid region, the river is heavily dependent on glacier meltwater, which provides about 71% of its flow. Some 20% comes from groundwater seepage, and only 9% comes from direct precipitation. Historical accounts suggest that the river may have reached the Tarim as recently as 200 B.C, when the climate in the area was wetter and much less water was being used by human activities.

Ning River

Ning River (Chinese: 宁江; pinyin: Níng Jiāng) is a tributary of Mei River. It originates and runs through Xingning, China.

Ruo Shui

Ruo Shui (Chinese: 弱水; literally: 'weak water', also Etsin Gol or Ruo He or Ejin River) is a major river system of northern China. It flows approximately 630 kilometres (390 mi) from its headwaters on the northern Gansu side of the Qilian Mountains north-northeast into the endorheic Ejin Basin in the Gobi Desert. The river forms one of the largest inland deltas or alluvial fans in the world. Its drainage basin covers about 78,600 square kilometres (30,300 sq mi) in parts of the Chinese provinces of Gansu and Inner Mongolia.

Salween River

The Salween or officially the Thanlwin River (Burmese:

သံလွင်မြစ်; IPA: [θàɴlwɪ̀ɴ mjɪʔ], Thai transcription: แม่น้ำสาละวิน), known in China as the Nu River (Tibetan: རྒྱལ་མོ་རྔུལ་ཆུ།, ZYPY: Gyämo Ngüqu; Chinese: 怒江; pinyin: Nù Jiāng) and in Sino-Burmese Daic area as Hong River (ᥑᥨᥒᥰ xoong or ၶူင်း xuung), is a river about 2,815 kilometres (1,749 mi) long that flows from the Tibetan Plateau into the Andaman Sea in Southeast Asia.

It drains a narrow and mountainous watershed of 324,000 square kilometres (125,000 sq mi) that extends into the countries of China, Burma and Thailand. Steep canyon walls line the swift, powerful and undammed Salween, one of the longest free-flowing rivers in the world. Its extensive drainage basin supports a biodiversity comparable with the Mekong and is home to about 7 million people. In 2003, key parts of the mid-region watershed of the river were included within the Three Parallel Rivers of Yunnan Protected Areas, a UNESCO World Heritage Site.The people who live on the Salween are relatively isolated from the rest of the world. The river is only navigable up to 90 kilometres (56 mi) from the mouth, and only in the rainy season.

The Burma Road was constructed between 1937 and 1938 during the Second Sino-Japanese War and crossed the river at the Huitong bridge. The Huitong bridge was blown by the retreating Chinese army and the river became the frontline from 1942 to 1944.

The Salween Campaign of World War II, was launched in order to liberate occupied China and open the Burma Road again and connect it to the Ledo Road.

Logging began on the mountains surrounding the Salween in the late 20th century, and has damaged the river's ecology. In recent years, there have been a number of proposals to dam the Salween River, both upstream in China and downstream in Myanmar, which have prompted social and environmental concerns as well as widespread opposition. Construction of at least one upstream dam on a tributary of the Salween is currently underway in China's Yunnan province, with many more expected to follow.

Shule River

The Shule River flows generally westwards through the Tibetan Plateau and the desert regions of northwestern China. It starts in the Qilian Mountains and stretches for some 900 kilometres (560 mi); however, the river dries up about two-thirds of the way along its course and is lost in the Kumtag Desert, an endorheic basin, meaning its water never reaches the sea. Historically, the river reached farther west to Lop Nur, an intermittent salt lake in the Taklimakan Desert. Large irrigation diversions off the river and the gradual desertification of the region have reduced its flow significantly.

Tarim River

The Tarim River (Chinese: 塔里木河; pinyin: Tǎlǐmù Hé; Uyghur: تارىم دەرياسى‎, ULY: Tarim deryasi), known in Sanskrit as the Śītā is an endorheic river in Xinjiang, China. It is the principal river of the Tarim Basin, a desert region of Central Asia between the Tian Shan and Kunlun Mountains. The river historically terminated at Lop Nur, but today reaches no further than Taitema Lake before drying out.

It is the longest inland river in China, with an annual flow of 4 to 6 billion cubic metres (3,200,000 to 4,900,000 acre⋅ft) or 158.5 cubic metres per second (5,600 cu ft/s). Its basin is home to nearly 10 million Uyghur and other ethnic minorities.

White Jade River

The White Jade River, also known by the native names Baiyu or Yurungkash, is a river in the southern Xinjiang region of China.The head waters of the river rise in the Kunlun Mountains, in the area of Aksai Chin in Kashmir in the Togatax area (35.6°N 81.4°E / 35.6; 81.4). The river flows east for some 200 km and then north for another 200 km before passing through Khotan, China (37.11°N 79.97°E / 37.11; 79.97). In Khotan, the river has yielded white river rocks which are also known as nephrite jade. North of Khotan, it eventually dries up in the Taklamakan desert, its seasonal bed joined by that of the Black Jade River (Karakash River) near Koxlax (some 200 km north of Khotan, 38.08°N 80.56°E / 38.08; 80.56), from where it continues north as the Hotan River, which flows into the Tarim River. The river drains an area of 14,575 km2 (5,627 sq mi) and has a discharge of 72.3 cubic metres per second (2,550 cu ft/s).

The river gets its name from the white jade that is often found in its alluvial deposits. The jade can also however be found in semi-shallow areas of the river..

Wu River (Yangtze tributary)

The Wu River (Chinese: 乌江; pinyin: Wū Jiāng) is the largest southern tributary of the Yangtze River. Nearly its entire length of 1,150 kilometres (710 mi) runs within the isolated, mountainous and ethnically diverse province of Guizhou. The river takes drainage from a 80,300-square-kilometre (31,000 sq mi) watershed.

The river flows through the Liupanshui, Anshun, Guiyang (the capital), Qiannan, and Zunyi Districts of Guizhou. All nine regions of the province have at least partial drainage to the river.

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