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The Li River or Li Jiang (Chinese: 漓江; pinyin: Lí Jiāng) is the name for the upper reaches of the Gui River in northwestern Guangxi, China. It is part of the Xijiang River system in the Pearl River Basin. The river flows 164 kilometres (102 mi) from Xing'an County to Pingle County, where the karst mountains and river sights highlight the famous Li River cruise.[1]

Li River
Native name漓江
Location
CountryChina
SubdivisionGuangxi
Physical characteristics
SourceMao'ershan
  locationXing'an County, Guangxi, China
  coordinates25.88°N 110.47°E / 25.88; 110.47
MouthGui River
  location
Pingle County, Guangxi, China
  coordinates
24.64°N 110.61°E / 24.64; 110.61
Length164 km (102 mi)
Discharge 
  locationGuilin
  average215 m3/s (7,600 cu ft/s)
Li River
"Li River" in Simplified Chinese characters
Traditional Chinese灕江
Simplified Chinese漓江

Background


The Li River originates in the Mao'er Mountains in Xing'an County and flows in the general southern direction through Guilin, Yangshuo and Pingle. In Pingle the Li River merges with the Lipu River and the Gongcheng River and continues south as the Gui River, which falls into the Xi Jiang, the western tributary of the Pearl River, in Wuzhou.

Tourist rafting boats cruise from Yangshuo County, on the Li River
Tourist rafting boats cruise from Yangshuo County, on the Li River

The upper course of the Li River is connected by the ancient Lingqu Canal with the Xiang River, which flows north into the Yangtze; this in the past made the Li and Gui Rivers part of a highly important waterway connecting the Yangtze Valley with the Pearl River Delta.

The 439-kilometre (273 mi) course of the Li and Gui Rivers is flanked by green hills. Cormorant fishing is often associated with the Lijiang (see bird intelligence).

Li River cruises from Guilin to Yangshuo are famous, attracting millions of visitors a year.[2]


Geology


Upper reaches of the Li River
Upper reaches of the Li River

The Li River and tributaries drain the area from Guilin to Yangshuo, descending from 141 m at Guilin to 103 m at Yangshuo. Mean flow past Guilin is 215 cubic metre per second, and alluvium sediments consisting of well sorted gravels covered by silty sand, form floodplains and terraces along its route. Yet, it is the 2,600 m of Devonian and Carboniferous limestones and karst terrain within the Guilin Basin, that gives the area a dramatic landscape. Two distinctive types of karst are found, Fengcong, and Fenglin, which have evolved for the past 10-20 million years, within the Cenozoic.[2]

Fog on the Li River
Fog on the Li River

Fengcong karst dominates the course of the Li River and is defined as a group of limestone hills with a common limestone base, with deep depressions or dolines between the peaks, and sometimes described as peak cluster depression karst. Hundreds of caves are present in this terrain, with 23 having passages longer than -1 km alongside the Li River gorge. The longest is the Guanyan Cave System which extends from Caoping to Nanxu.[2]

Fenglin dominates the area around Yangshuo and south of Guilin and is defined as isolated limestone hills separated by a flat limestone surface generally covered by loose sediments, and sometimes described as a peak forest plain. The best-known fenglin is the tower karst around Yangshuo. These towers consist of strong and massive limestone forming near vertical sides with base diameters less than 1.5 times their height. The heights of the towers range from 30 to 80 m in the central basin but can be as high as 300 m near the Fengcong. Fenglin evolves from Fengcong by slow and continuous tectonic uplift, associated with the Himalayan orogenic zone, and even slower erosion of the towers.[2]

Famous Show caves in the Guilin area include Qixing Dong and Luti Dong.[2]


Notable features


Fishing boat on the Li River
Fishing boat on the Li River
  1. Reed Flute Cave: a limestone cave with a large number of stalactites, stalagmites, stalacto-stalagmites, rocky curtains, and cave corals.
  2. Seven-Star Park: the largest park in Guilin.
  3. Mountain of Splendid Hues: a mountain consisting of many layers of variously colored rocks.
  4. Elephant-Trunk Hill: a hill that looks like a giant elephant drinking water with its trunk. It is a symbol of the city of Guilin.
  5. Lingqu Canal: dug in 214 BC, is one of ancient China's three big water conservation projects and the oldest existing canal in the world.
  6. Other attractions include Duxiu Peak, Nanxi Park, the Taohua River, the Giant Banyan, and the Huashan-Lijiang National Folklore Park.

The imagery of the Li River is featured in the fifth series of the 20 yuan note.



Guilin

See also



References


  1. "Li River Cruises". Retrieved 2022-03-25.
  2. Waltham, Tony (2010). Migon, Piotr (ed.). Guangxi Karst: The Fenglin and Fengcong Karst of Guilin and Yangshuo, in Geomorphological Landscapes of the World. Springer. pp. 293–302. ISBN 9789048130542.


На других языках


[de] Li Jiang

Der Li Jiang oder Li-Fluss (chinesisch .mw-parser-output .Hani{font-size:110%}漓江, Pinyin Lí Jiāng) ist ein 437 Kilometer langer Fluss im Autonomen Gebiet Guangxi der Zhuang in der Volksrepublik China.
- [en] Li River

[es] Río Li

El río Li (en chino simplificado, 漓江; pinyin, Lí Jiāng, de ahí que en ocasiones aparezca referido como río Lijiang) es un destacado afluente de la cuenca del río de las Perlas que discurre íntegramente en la Región Autónoma de Guangxi, en la República Popular China. El sistema Li-Gui tiene una longitud de 437 km y drena una cuenca de 19 025 km², similar a países como El Salvador, Israel o Eslovenia.

[it] Lijiang (fiume)

Il Lijiang o Li Jiang (cinese: 漓江S, LíjiāngP, fiume Li) è un fiume della Regione Autonoma di Guangxi Zhuang, nella Cina meridionale. Ha origine dai monti Mao'er, nella contea Xing'an e attraversa le città di Guilin e Yangshuo per immettersi, a Wuzhou, nel fiume Xi Jiang, che è a sua volta uno dei tre immissari del fiume delle Perle, assieme al Beijiang e al Dongjiang.

[ru] Гуйцзян

Гуйцзян (кит. 桂江; Лицзян[1], Лишуй[1]) — река в Гуанси-Чжуанском автономном районе КНР, является одним из основных истоков реки Сицзян (Западная река). Начинается в уезде Синъань, в северо-восточном углу района (городской округ Гуйлинь).



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