Tarim River

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Formed from the union of the Aksu River and Yarkand River, it flows in an eastward direction around the Taklamakan Desert. The Muzat River is one of its tributaries.

The Chinese originally considered the Tarim to be the upper course of the Huanghe or Yellow River [http://depts.washington.edu/silkroad/texts/hhshu/notes2.html#2_1 Notes to the draft annotated translation of the 'Chapter on the Western Regions' from the "Hou Hanshu" (2003) by John E. Hill] but, by the time of the Former Han Dynasty (125 BCE-23 CE), it was known that it drains into Lop Nur, a series of salt lakes. [A. F. P. Hulsewé and M. A. N. Loewe, "China in Central Asia: The Early Stage: 125 B.C.-A.D. 23". Leiden E. J. Brill (1979) ISBN 90-04-05884-2] Its total length is 2,030 km (or 1,260 mi).

It is the longest inland river in China with an annual flow of 4-6 billion cubic meters. Its valley is home to nearly 10 million Chinese and other ethnic minorities including Uyghurs and Mongolians.

It is shallow, unsuitable for navigation, and because of its heavy silt load, forms a braided stream near its terminus at the Godzareh depression. It gives its name to the arid Tarim Basin.

It lies immediately north of the Tibetan Plateau. The river gives its name to the great Tarim Basin between the Tian Shan and Kunlun Mountains systems of Central Asia. It flows for most of its length through the Taklamakan Desert. The word 'tarim' is used to designate the bank of a river that flows into a lake or that is not able to be differentiated from the sands of a desert. This is a characteristic hydro graphic feature of many rivers that traverse the sands of the Taklamakan Desert. Another characteristic of the rivers of the Tarim Basin, including the Tarim River itself, is their active migration, that is, the shifting of their beds and banks.

The Tarim River is formed by the confluence of the Kashgar River and the Yarkand River in the far west; flowing northeastward from this confluence, the river is then joined some 370 km (230 mi) downstream by the Aksu and the Khotan rivers. Only the Aksu River flows for the entire year. It is the Tarim's most important tributary, supplying 70–80 percent of its water volume. The name Tarim is used below the Khotan River confluence. The total length of the Yarkand-Tarim river system is 2,030 km (1,261 mi), although, as the Tarim frequently changes its channel, the length tends to vary over the years. Prior to the completion of reservoirs and irrigation works in the mid-20th century, the Tarim's waters eventually reached Lop Nur (now a salt-encrusted lake bed). The river's waters now drain intermittently into Taitema Lake, which is located about 160 km (100 mi) southwest of Lop Nur. The area of the Tarim River Basin is about 557,000 square km (215,000 square mi). A considerable part of the Tarim's course is unformed, following no clearly defined riverbed. The water volume of the lower course of the river diminishes as a result of extensive evaporation and water-diversion schemes. The Tarim's low-water period is from October through April. The spring and summer high waters begin in May and continue through September as the snows melt on the distant Tian Shan and Kunlun mountains.

The Lower Tarim Basin is an arid plain composed of alluvium and lake sediments and is bordered by massive mountain ranges. The basin is the driest region of Eurasia. The predominant part of it is occupied by the Taklamakan Desert, whose sand area exceeds 270,000 square km (105,000 square mi). In addition, there are several comparatively small sand massifs with areas of from 780 to 4,400 square km (300 to 1,700 square mi). Sand dunes are the predominant relief.

Precipitation in the Tarim Basin is extremely scanty, and in some years it is nonexistent. In the Taklamakan Desert and in the Lop Nur basin, the average annual total of precipitation is about 12 mm (0.5 in). In the foothills and in several other areas of the river's basin, the precipitation amounts to from 50 to 100 mm (2 to 4 inches) a year. In the Tian Shan it is much wetter, precipitation often exceeding 20 inches (500 mm). Maximum temperatures in the Tarim Basin are about 40° C (104° F). The Tarim River freezes over every year from December through March.

Vegetation in the Tarim Basin is mainly located along the river and its branches. There, at the edge of the sands, shrub like vegetation and stunted trees, especially wormwood, are found. A thin forest of poplar grows in the Tarim River valley. Underbrush consists of willows, sea buckthorn, and dense growths of Indian hemp and Ural licorice.

The Tarim River is rich in fish, and animal life on the river and the surrounding desert is varied. The valley and lakes of the Tarim are a stopover for many migratory birds.

Despite the Chinese government's promotion of large-scale irrigation, oasis agriculture remains the mainstay of the scattered settlements in the region. Grains, cotton, silk, fruits, and wool are the chief agricultural products, and Khotan jades are the only other important item. Little is exported from the basin, but local surpluses find a market among travelers passing through when conditions permit.

Chinese authorities in the northwestern region of Xinjiang are relocating hundreds of ethnic minority farming families along the dwindling Tarim River. By 2008, more than 6,000 households along the river will have been resettled and cultivation forbidden along the river banks, in an attempt to save 60 million cubic meters (16 billion gallons) of water.

Footnotes

References

*Hill, John E. 2003. "Annotated Translation of the Chapter on the Western Regions according to the "Hou Hanshu"." 2nd Draft Edition. [http://depts.washington.edu/silkroad/texts/hhshu/hou_han_shu.html]
*Hill, John E. 2004. "The Peoples of the West from the Weilüe" 魏略 "by Yu Huan" 魚豢": A Third Century Chinese Account Composed between 239 and 265 CE." Draft annotated English translation. [http://depts.washington.edu/silkroad/texts/weilue/weilue.html]
*Hulsewé, A. F. P. and Loewe, M. A. N. 1979. "China in Central Asia: The Early Stage 125 BC – AD 23: an annotated translation of chapters 61 and 96 of the History of the Former Han Dynasty". E. J. Brill, Leiden.
*Stein, Aurel M. 1907. "Ancient Khotan: Detailed report of archaeological explorations in Chinese Turkestan", 2 vols. Clarendon Press. Oxford. [http://dsr.nii.ac.jp/toyobunko/]
*Stein, Aurel M. 1921. "Serindia: Detailed report of explorations in Central Asia and westernmost China", 5 vols. London & Oxford. Clarendon Press. Reprint: Delhi. Motilal Banarsidass. 1980. [http://dsr.nii.ac.jp/toyobunko/]

uggested reading

*Baumer, Christoph. 2000. "Southern Silk Road: In the Footsteps of Sir Aurel Stein and Sven Hedin". White Orchid Books. Bangkok.
*Mallory, J.P. and Mair, Victor H. 2000. "The Tarim Mummies: Ancient China and the Mystery of the Earliest Peoples from the West". Thames & Hudson. London.

ee also

* Geography of China

External links

* [http://earthtrends.wri.org/maps_spatial/maps_detail_static.cfm?map_select=373&theme=2 Information and a map of the Tarim's watershed]
* [http://depts.washington.edu/uwch/silkroad/ Silk Road Seattle] (The Silk Road Seattle website contains many useful resources including a number of full text historical texts)
* [http://www.drben.net/ChinaReport/Sources/China_Maps/Map-Satellite-Tarim_River_Basin-Taklamakan_Desert-1A.html Satellite Image Based Map of the Tarim River Basin and Taklamakan Desert + Surrounding Mountain Ranges]
* [http://china.notspecial.org/gallery/album30/ Photos of the Tarim River] (from a Xinjiang blog)