Rivers of China
China¡¯s Major Rivers
Yangtze River is the longest river of Asia, about 6300 km (about 3937 mile) in length. It rises in the Kunlun Mountains in the southwestern section of Qinghai Province in China, and flows generally south through Sichuan Province into Yunnan Province, where, in the vicinity of Huize, it bends sharply to the northeast. Then, it flows generally northeast and east across central China through Sichuan, Hubei, Anhui, and Jiangsu Provinces to its mouth in the East China Sea, about 23 km (about 14 mi) north of Shanghai.
The headwaters of the Yangtze are situated at an elevation of about 4900 m (about 16,000 ft). In its descent to sea level, the river falls to an altitude of 305 m (1000 ft) at Yibin, Sichuan Province, the head of navigation for riverboats, and to 192 m (630 ft) at Chongqing. Between Chongqing and Yichang (I-ch'ang), at an altitude of 40 m (130 ft) and a distance of about 320 km (about 200 mi), it passes through the spectacular Yangtze Gorges, which are noted for their natural beauty but are dangerous to shipping. Yichang, 1600 km (1000 mi) from the sea, is the head of navigation for river steamers; oceangoing vessels may navigatethe river to Hankou (Hankow), a distance of almost 1000 km (almost 600 mi) from the sea. For about 320 km (about 200 mi) inland from its mouth, the river is virtually at sea level.
More than 1,683,500 sq km (650,000 sq mi) of territory is drained by the Yangtze and its branches. The principal tributaries are the Han, Yalong, Jialing, Min, and Tuo He (T'o Ho), on the N and on the south, the Wu; at Zhenjiang, the Grand Canal links the Yangtze to the Huang He (yellow River). During periods of heavy rains, Lakes Dongting and Poyang receive some of the overflow of the Yangtze. Despite these outlets, floods caused by the river occasionally have caused great destruction of life and property. In the 20th century, devastating floods have occurred in 1905, 1980, and 1981.
With its numerous tributaries and feeders, the Yangtze provides a great transportation network through the heart of some of the most densely populated and economically important areas in China. Among the principal cities on the Yangtze, in addition to those cited in the foregoing, are Wuchang, Nanjing, Hanyang, and Anqing (An-ch'ing). Jiangsu Province, largely a deltaic plain consisting of silt deposited by the Yangtze (more than 170 million cu m/6 billion cu ft annually), is one of the chief rice-growing areas of China.
Although the entire river is known as the Yangtze River to foreigners, the Chinese apply that designation only to the last 480 or 645 km (300 or 400 mi) of its course, the portion traversing the region identified with the Yang kingdom (flourished about 10th century BC). From Its upper reaches to Yibin, the river is called the Jinsha River (Golden Sand) and various other names are applied in the provinces it traverses. The official name for the entire river is Chang Jiang ("Long River) or Yangtze River.The Yellow
4,827 km-long Huanghe (yellow river) originates from Kunlun Mountains
and flows generally eastward across northern China to the Gulf of Bo Hai.
Passing Cities :Anyang \ Jinan \Kaifeng\Lanzhou \Luoyang \Sanmenxia\ Wuzhong \Yanjin\ ZhengzhouHeilong
Jiang (Amur River) is the northernmost major stream of China. It forms
most of the northeastern boundary with Russia. It is a major fishing resource
in north China.
Zhujiang (the Pearl) River is the largest river in south China, formed
but the confluence of three rivers---the Xijiang, Beijiang and Dongjaing.
Its name comes from pearl shells having been found in the section that
flows through the city of Guangzhou. The Xijiang, the trunk of the Zhujiang
(Pearl River), has its headwaters in the Nanpan River in the Wumeng Mountain
Area, Yunnan, and flows past Yunnan, Guizhou and Guangxi for 2,197 kilometers
before emptying into the South China Sea at Modaomen, Guangdong. Seventy-seven
percent of Zhujiang (Pearl River) flow comes from the Xijiang. Practically
all the rivers of the Beijinga and dongjaing systems are in Guangdong
Province. The Beijiang, starting in the southern part of Huanan and Jiangxi,
flows 468 kilometers. The Dongjiang has its source in southern Jiangxi
and a total length of 523 kilometers. The three rivers meet at the Zhujiang
River (Pearl River) Delta formed of the silt deposits at the river mount,
where they fan out and flow into the South China Sea through eight outlets,
mainly those at Humen, Hongqili, Modaomen and Yamen. The Zhujiang (Pearl
River) valley, which covers an area of 452,616 square kilometers, has
an annual precipitation of 1,500-2,000 mm. and is the region with the
largest rainfall. In length and catchment area, the Zhujiang (Pearl River)
ranks fourth among China's rivers, but its flow, eight times that of the
Huanghe, is second only to the Yangtze River and provides it with a power
potential of 33 million kilowatts. It is second also to the Yangtze River
in the volume of water transport, its trunk and branch rivers being navigable
for a total length of 12,000 kilometers. It is navigable by ships of 10,000-ton
class downriver form the Hangpu port near Guangzhou, by 1,000-tonners
up to Wuzhou and by small steamboats up to Nanning and Liuzhou. Farming
is well developed in the Zhujiang (Pearl River) basin. The Zhujiang River
(Pearl River) Delta has a network of rivers, fertile soil, abundant natural
resources and a sense population.
Zhujiang originates from Xijiang, one of the largest river system
in south China. Nicked named "Pearl River", Zhujiang is the
pearl of South China, fostering booming cities such as Guangzhou, Zhuhai,
Jiangmen in the entire delta region.
Despite its size, Lancang offers a few places to spend the night. This is also a good place to sample traditional home cooking and hospitality. Those with time to kill can hire a bicycle to explore the surrounding area or simple wander around the town and relax beside the river. It is also possible to take a short boat trip along the river to the next town and back again.
The Yarlung Zangbo River, an international water system, is located at the Tibet Autonomous Region and a river with the highest altitude in the world. The total length of the Yarlung Zangbo River in China is 2,057 kilometers, ranking the 5th longest river among the famous rivers of China. It has a drainage area of 240,480 square kilometers, and ranks the 6th largest river in China. Its annual runoff volume to foreign country is 140 billion m3, ranking the 3rd largest in China, just next to the Yangtze River and the Pearl River.
Location: Situated in the northwest of Yunnan Province, Nujiang Lisu Autonomous Prefecture neighbors Lijiang City,Diqingand Dali prefectures in the east. It is also bordered by Tibet in the north and shares a boundary of nearly 450 kilometers (280 miles) with Burma in the west.
Being one of the largest rivers in northern China, the Liaohe River is called the Mother River by people in Liaoning Province. Originated in Qilaotu Mountain in Heibei Province, it flows 1,394 kilometers through Hebei, Inner Mongolia, Jilin, and Liaoning provinces, and at last empties into the Bohai Sea, with a drainage area of 201,600 square kilometers.
The upper reaches of the river stretch 882 kilometers, running through loess hills; the middle reaches stretch 210 kilometers, to the Stone Buddha Temple; and the lower reaches have 302 kilometers.
The river abounds in precipitation rainfall especially in summer, which often causes serious floods in the lower reaches. Besides, the most challenging engineering aspect of taming the Liaohe River is the control of the exceptionally high sediment load that the river carries in its lower reaches, with 20.98 million tons of sediment on the average entering the river channel annually, only next to the Yellow River and the Haihe River.
The Haihe, the largest water system in north china, is formed by five large rivers¡ªthe North Canal, the Yongding, the Daqing, the Ziya and the South Canal¡ªand more than 300 tributaries these spread out like a palm-leaf fan over the vast areas in north China and converge near Tianjin to form the Haihe, which then flows east and empties into the Bohai Sea at Dagukou. This 69-kilometer trunk of the Haihe from Tianjin to Dagukou is like the handle of the fan, channeling the more than 300 tributaries into the sea. The Haihe basin covers Beijing, Tianjin, the greater part of Hebei, and parts of Shandong, Henan, Shanxi and Inner Mongolia. It has a catchment area of 265,000 square kilometers and 180 million mu of farmland. The Haihe has its source in the Weihe river and total length of 1,090 kilometers.
The rainy season is concentrated in a very short period in the Haihe valley. When heavy rains occur, the torrents of the numerous tributaries in the upper reaches rush into lwo-lying middle and lower reaches, where the river is narrow and there is only one outlet to the sea, causing it to burst onto the plain in treat floods. The city of Tianjin was inundated on more than 70 occasions in the 500 years or more before 1949. In a major flood in 1939, vast areas in the North China Plain were submerged, and the water in the streets in Tianjin were two meters deep, so that boats were the only means of transport for upwards of two months. In 1963, the Haihe basin was hit by a flood with out parallel in history. In eh following decade or more, comprehensive measures have been taken to bring the river under permanent control. More than 1,580 reservoirs and 4,3000 kilometers of dykes have been built, the river channels have been dredge, and 10 additioanl outlets to the sea have been opened, raising the flood-diversion capacity more than 10 times. Now the Haihe basin is basically free from the menace of floods.
The Huaihe, an important river in central China, flows from west to east, with the Huanghe in the north and Yangtze River in the south. Starting in the Tongbai Mountains in Henan, it has its upper reaches in Henan, its middle reaches in Anhui and its lower reaches in Jiangsu. Its trunk is about 1,000 kilometers long and its catchment area about 185,700 square kilometers. The Huaihe basin is mostly plain and has a cultivated area of more than 200 million mu.The Huaihe had its outlet to the sea about eight centuries ago. In 1194, the Huanghe breached its own dykes and merged with the downriver course of the Huaihe. Before it reverted to its old course in mid-19th century, the Huanghe had deposited large amounts of mud and silt in the lower reaches of the Huaihe and sealed up the latter¡¯s outlet to the sea. With the passage of time, the waters of the Huaihe converged to form two large lakes, Hongze and Gaoyou. In its high-water season the Huaihe flows through the Honze and Gaoyou lakes and the Grand Canal into the Yangtze River near Yangzhou before emptying into the sea. Because its lower reached its dykes and caused 250 major floods in the five centuries or more before 1949. Since the birth of the People¡¯s Republic of China in 1949, many reservoirs and flood-detention projects have been built in its upper and middle reaches, new courses have been laid out in its lower reaches and its outlet to the sea has been widened. In this way, the greater part of its water now flows into the Yangtze River and the rest into the Huanghai Sea through the new channels. Today, the Huaihe basin has an irrigated area of about 100 million mu, and the disaster-ridden, low yielding region is on its way to prosperity.
Yili Kazak autonomous prefecture (shortened as Yili prefecture) situates in the northwest border of People¡¯s Republic of China, also in the northwestern part of Xinjiang Uighur autonomous region. It borders Russia and Mongolia in the northeast, and it connects Changji Hui Autonomous Prefecture and Bayinguoleng Mongol autonomous prefecture in the southeast. It faces Akesu area in the southwest, and it borders the Republic of Kazakhstan in the northwest.
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