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The Amu Darya ( ; ), also shortened to Amu and historically known as the Oxus ( ), is a major river in which flows through , , , and . Rising in the , north of the , the Amu Darya is formed by the confluence of the and rivers, in the Tigrovaya Balka Nature Reserve on the border between Afghanistan and , and flows from there north-westwards into the southern remnants of the . In its upper course, the river forms part of Afghanistan's northern border with Tajikistan, , and . In , the river was regarded as the boundary of with , which roughly corresponded to present-day Central Asia.B. Spuler, Āmū Daryā, in Encyclopædia Iranica, online ed., 2009 The Amu Darya has a flow of about 70 cubic kilometres per year on average.


Names
In classical antiquity, the river was known as the Ōxus in and (Ôxos) in Greek — a clear derivative of , the name of the largest tributary of the river. In , the river is also referred to as Vakṣu (वक्षु). The refers to the river as Chaksu (चक्षु) which means 'an eye' in sanskrit. The texts too refer to the river as Yakhsha/Vakhsha (and Yakhsha Arta ('Upper Yakhsha'), referring to the / twin river to Amu Darya). In sources of the the river is known as Wehrōd ().

The name Amu is said to have come from the medieval city of Āmul (later Chahar Joy/Charjunow, and now known as Türkmenabat) in modern , with Daryā being the Persian word for 'lake' or 'sea'.


Identification with the Gihon
Medieval and sources call the river Jeyhoun (), which is derived from , the for one of the four rivers of the Garden of Eden.William C. Brice. 1981. Historical Atlas of Islam (Hardcover). Leiden with support and patronage from Encyclopaedia of Islam. . The Amu Darya passes through one of the world's highest deserts.


As the river Gozan
Western travelers in the 19th century mentioned that one of the names by which the river was known in Afghanistan was Gozan, and that this name was used by Greek, Mongol, Chinese, Persian, Jewish, and Afghan historians. However, this name is no longer used.

"Hara () and to the river of Gozan (that is to say, the Amu, (called the Oxus by Europeans )) ..."

"the Gozan River is the River Balkh, i.e. the Oxus or the Amu Darya ..."

"... and were brought into Halah (modern day ), and Habor (which is Pesh Habor or ), and Hara (which is ), and to the river Gozan (which is the Ammoo, also called Jehoon) ..."


Description
The river has a total length of , and its drainage basin covers , providing a mean discharge of about of water per year. The river is navigable for over . All of the water comes from the high mountains in the south where annual can be over . Even before large-scale irrigation began, high summer evaporation meant that not all of this discharge reached the – though there is some evidence the large Pamir provided enough for the Aral to overflow during the 13th and 14th centuries.

Since the end of the 19th century, there have been four different claimants as the true source of the Oxus:

A glacier turns into the and joins the Pamir River about downstream. Bill Colegrave's expedition to Wakhan in 2007 found that both claimants 2 and 3 had the same source, the Chelab stream, which bifurcates on the watershed of the Little Pamir, half flowing into Lake Chamaktin and half into the parent stream of the Little Pamir/Sarhad River. Therefore, the Chelab stream may be properly considered the true source or parent stream of the Oxus.
(2025). 9781903071281, Bene Factum Publishing. .
The Panj River forms the border of and . It flows west to Ishkashim where it turns north and then north-west through the passing the Tajikistan–Afghanistan Friendship Bridge. It subsequently forms the border of Afghanistan and Uzbekistan for about , passing and the Afghanistan–Uzbekistan Friendship Bridge. It delineates the border of Afghanistan and Turkmenistan for another before it flows into Turkmenistan at . It flows across Turkmenistan south to north, passing Türkmenabat, and forms the border of Turkmenistan and Uzbekistan from Halkabat. It is then split by the Tuyamuyun Hydro Complex into many waterways that used to form the joining the Aral Sea, passing , Daşoguz, and other cities, but it does not reach what is left of the sea any more and is lost in the desert. Use of water from the Amu Darya for has been a major contributing factor to the shrinking of the Aral Sea since the late 1950s. Historical records state that in different periods, the river flowed into the (from the south), into the (from the east), or both, similar to the (Jaxartes, in ). Partly based on such records, first and later engineers proposed to divert the Amu Darya to the Caspian Sea by constructing the Transcaspian Canal.
(2025). 9781108468541, Cambridge University Press. .


Watershed
The of the Amu Darya include most of Tajikistan, the southwest corner of , the northeast corner of Afghanistan, a narrow portion of eastern Turkmenistan and the western half of Uzbekistan. Part of the Amu Darya basin in Tajikistan forms that country's border with China (in the east) and Pakistan (to the south). About 61% of the drainage lies within Tajikistan, Uzbekistan and Turkmenistan, while 39% is in Afghanistan.

The abundant water flowing in the Amu Darya comes almost entirely from in the and , which, standing above the surrounding arid plain, collect atmospheric moisture which otherwise would probably escape elsewhere. Without its mountain water sources, the Amu Darya would not exist—because it rarely rains in the lowlands through which most of the river flows. Of the total drainage area, only about actively contribute water to the river. This is because many of the river's major tributaries (especially the ) have been diverted, and much of the river's drainage is arid. Throughout most of the steppe, the annual rainfall is about .


History
The ancient called the Amu Darya the Oxus. In ancient times, the river was regarded as the boundary between and (). The river's drainage lies in the area between the former empires of and Alexander the Great, although they occurred at very different times. When the Mongols came to the area, they used the water of the Amu Darya to flood . One southern route of the ran along part of the Amu Darya northwestward from before going westwards to the .

According to the Quaternary International, it is possible that the Amu Darya's course across the has gone through several major shifts in the past few thousand years. Much of the time – most recently from the 13th century to the late 16th century – the Amu Darya emptied into both the Aral and the Caspian Seas, reaching the latter via a large called the . The Uzboy splits off from the main channel just south of the river's delta. Sometimes the flow through the two branches was more or less equal, but often most of the Amu Darya's flow split to the west and flowed into the Caspian.

People began to settle along the lower Amu Darya and the Uzboy in the 5th century, establishing a thriving chain of agricultural lands, towns, and cities. In about AD 985, the massive Gurganj Dam at the bifurcation of the forks started to divert water to the Aral. 's troops destroyed the dam in 1221, and the Amu Darya shifted to distributing its flow more or less equally between the main stem and the Uzboy. But in the 18th century, the river again turned north, flowing into the Aral Sea, a path it has taken since. Less and less water flowed down the Uzboy. When Russian explorer Bekovich-Cherkasski surveyed the region in 1720, the Amu Darya did not flow into the Caspian Sea anymore.

By the 1800s, the ethnographic makeup of the region was described by as the communities of "the vassal Khanates of Maimene, Khulm, Kunduz, and even the Badakshan and Wahkran." An Englishman, William Moorcroft, visited the Oxus around 1824 during the period.Peter Hopkirk, The Great Game, 1994, page 100 Another Englishman, a naval officer called John Wood, came with an expedition to find the source of the river in 1839. He found modern-day , called it Lake Victoria, and proclaimed he had found the source.Keay, J. (1983) When Men and Mountains Meet Chapter 9 Then, the French explorer and geographer Thibaut Viné collected a lot of information about this area during five expeditions between 1856 and 1862.

The question of finding a route between the Oxus valley and India has been of concern historically. A direct route crosses extremely high mountain passes in the and isolated areas like . Some in Britain feared that the Empire of Russia, which at the time wielded great influence over the Oxus area, would overcome these obstacles and find a suitable route through which to invade – but this never came to pass.See for example Can Russia invade India? by Henry Bathurst Hanna, 1895, (Google eBook), or The Káfirs of the Hindu-Kush, Sir George Scott Robertson, Illustrated by Arthur David McCormick, Lawrence & Bullen, Limited, 1896, (Google eBook) The area was taken over by Russia during the Russian conquest of Turkestan.

The became the ruling power in the early 1920s and expelled Mohammed Alim Khan. It later put down the Basmachi movement and killed . A large refugee population of Central Asians, including Turkmen, Tajiks, and Uzbeks, fled to northern Afghanistan.Taliban and Talibanism in Historical Perspective, M Nazif Shahrani, chapter 4 of The Taliban And The Crisis of Afghanistan, 2008 Harvard Univ Press, edited by Robert D Crews and Amin Tarzi In the 1960s and 1970s the Soviets started using the Amu Darya and the Syr Darya to irrigate extensive fields in the Central Asian plain. Before this time, water from the rivers was already being used for agriculture, but not on this massive scale. The , Karshi Canal, and Bukhara Canal were among the largest of the irrigation diversions built. However, the Main Turkmen Canal, which would have diverted water along the dry Uzboy River bed into central Turkmenistan, was never built. In the course of the Soviet–Afghan War in the 1970s, Soviet forces used the valley to invade Afghanistan through .Termez – See the Soviet–Afghan War article The Soviet Union fell in the 1990s and Central Asia split up into the many smaller countries that lie within or partially within the Amu Darya basin.

During the Soviet era, a resource-sharing system was instated in which and shared water originating from the Amu and with , , and in summer. In return, and received Kazakh, Turkmen, and Uzbek coal, gas, and electricity in winter. After the fall of the Soviet Union this system disintegrated and the Central Asian nations have failed to reinstate it. Inadequate infrastructure, poor water management, and outdated irrigation methods all exacerbate the issue.International Crisis Group. " Water Pressures in Central Asia ", CrisisGroup.org. 11 September 2014. Retrieved 6 October 2014.


Siberian Tiger Introduction Project
The used to occur along the river's banks.
(1992). 9789004088764, Smithsonian Institution and the National Science Foundation. .
After its extirpation, the Amu Darya's delta was suggested as a potential site for the introduction of its closest surviving relative, the . A feasibility study was initiated to investigate if the area is suitable and if such an initiative would receive support from relevant decision makers. A viable tiger population of about 100 animals would require at least of large tracts of contiguous habitat with rich prey populations. Such habitat is not available at this stage and cannot be provided in the short term. The proposed region is therefore unsuitable for the reintroduction, at least at this stage.Jungius, H., Chikin, Y., Tsaruk, O., Pereladova, O. (2009). Pre-Feasibility Study on the Possible Restoration of the Caspian Tiger in the Amu Darya Delta . WWF Russia


Resource extraction
Since March 2022, the building of the 285 km Qosh Tepa Canal has been underway in northern to divert water from the Amu Darya. has expressed concern that the canal will have an adverse effect on its agriculture. The canal is also expected to make the disaster worse, and in 2023 Uzbek officials held talks on the canal with the Taliban. The Taliban has made the canal a priority, with images supplied by demonstrate that from April 2022 to February 2023, more than 100 km of canal was excavated. According to the Taliban, the initiative is expected to convert 550,000 hectares of desert into farmland.

In January 2023, the Xinjiang Central Asia Petroleum and Gas Company (aka CAPEIC) signed a $720 million four-year investment deal with the government of for extraction on its side of the Amu Darya basin. The deal will see a 15% royalty given to the Afghan government over the course of its 25-year term. The Chinese see this basin as the third-largest potential gas field in the world.


Literature
The Oxus river, and Arnold's poem, fire the imaginations of the children who adventure with ponies over the moors of the West Country in the 1930s children's book The Far-Distant Oxus. There were two sequels, Escape to Persia and Oxus in Summer.

Robert Byron's 1937 travelogue, The Road to Oxiana, describes its author's journey from the through to , with the Oxus as his stated goal, "to see certain famous monuments, chiefly the Gonbad-e Qabus, a tower built as a mausoleum for an ancient king."

George MacDonald Fraser's Flashman at the Charge (1973), places Flashman on the Amu Darya and the Aral Sea during the (fictitious) Russian advance on India during The Great Game period. 's Halfway House to Heaven (2010), describes the 2007 expedition that finally determined the true source of the river.


See also


Notes

Further reading
  • Curzon, George Nathaniel. 1896. The Pamirs and the Source of the Oxus. Royal Geographical Society, London. Reprint: Elibron Classics Series, Adamant Media Corporation. 2005. (pbk; (hbk).
  • Gordon, T. E. 1876. The Roof of the World: Being the Narrative of a Journey over the high plateau of Tibet to the Russian Frontier and the Oxus sources on Pamir. Edinburgh. Edmonston and Douglas. Reprint by Ch'eng Wen Publishing Company. Taipei. 1971.
  • Toynbee, Arnold J. 1961. Between Oxus and Jumna. London. Oxford University Press.
  • Wood, John, 1872. A Journey to the Source of the River Oxus. With an essay on the Geography of the Valley of the Oxus by Colonel Henry Yule. London: John Murray.


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