Amu Darya: Difference between revisions
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{{Infobox_River |
{{Infobox_River |
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|river_name = Amu |
|river_name = Amu River |
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|image_name = amu darya delta.jpg |
|image_name = amu darya delta.jpg |
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|caption = |
|caption = Amudarya Delta from space, November 1994 |
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|origin = [[Pamir Mountains]] |
|origin = [[Pamir Mountains]] |
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|mouth = None, formerly [[Aral Sea]] |
|mouth = None, formerly [[Aral Sea]] |
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The '''Amu River''' ( |
The '''Amu River''' ({{lang-tg|дарёи Ому}} - ''Daryoi Omu'', [[Dari (Eastern Persian)|Dari]]: آمودریا - ''Âmudaryâ'', {{lang-ps|د آمو سيند}} - ''də Āmu Sind'', {{lang-uz|''Amudaryo''}}, {{lang-tk|Amyderýa}}), also called '''Oxus River''' or '''Amudarya River''', is a major river in [[Central Asia]]. It is formed by the junction of the [[Vakhsh River|Vakhsh]] and [[Panj River|Panj]] rivers. |
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== Names == |
== Names == |
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[[Image:Bridge.Amu.Darya.Urgench.jpg|left|thumb|Pontoon Bridge on the Amu |
[[Image:Bridge.Amu.Darya.Urgench.jpg|left|thumb|Pontoon Bridge on the Amu River near [[Urgench]]]] |
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Amu is said to have come from the city of Āmul, now known as [[Türkmenabat]]. Many local people refer to the river as '' [[Jayhoun]] '' (جيحون) which was thought to be a derivative of ''[[Gihon]]'', the biblical name for one of the four rivers of the [[Garden of Eden]] or [[paradise]].<ref name="ref1">William C. Brice. 1981. ''Historical Atlas of Islam (Hardcover)''. Leiden with support and patronage from Encyclopaedia of Islam. ISBN 90-04-06116-9.</ref> The river is also known by this name to most of the medieval Islamic writers. |
Amu is said to have come from the city of Āmul, now known as [[Türkmenabat]]. Many local people refer to the river as '' [[Jayhoun]] '' (جيحون) which was thought to be a derivative of ''[[Gihon]]'', the biblical name for one of the four rivers of the [[Garden of Eden]] or [[paradise]].<ref name="ref1">William C. Brice. 1981. ''Historical Atlas of Islam (Hardcover)''. Leiden with support and patronage from Encyclopaedia of Islam. ISBN 90-04-06116-9.</ref> The river is also known by this name to most of the medieval Islamic writers. |
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The river is navigable for over 1450 km (800 miles). Its total length is 2400 km (1500 miles) and its drainage basin totals {{convert|534739|km2|sqmi}} in area, providing a mean discharge of around {{convert|97.4|km3|cumi|lk=on}}<ref name="autogenerated1" /> of water per year. All of the water comes from the high mountains in the south where annual [[precipitation (meteorology)|precipitation]] can be over {{convert|1000|mm|in|abbr=on}}. Even before large-scale irrigation began, high summer evaporation meant that not all of this discharge reached the [[Aral Sea]] - though there is some evidence the large Pamir [[glacier]]s provided enough melt water for the Aral to overflow during the thirteenth and fourteenth centuries A.D. |
The river is navigable for over 1450 km (800 miles). Its total length is 2400 km (1500 miles) and its drainage basin totals {{convert|534739|km2|sqmi}} in area, providing a mean discharge of around {{convert|97.4|km3|cumi|lk=on}}<ref name="autogenerated1" /> of water per year. All of the water comes from the high mountains in the south where annual [[precipitation (meteorology)|precipitation]] can be over {{convert|1000|mm|in|abbr=on}}. Even before large-scale irrigation began, high summer evaporation meant that not all of this discharge reached the [[Aral Sea]] - though there is some evidence the large Pamir [[glacier]]s provided enough melt water for the Aral to overflow during the thirteenth and fourteenth centuries A.D. |
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One source of the Amu |
One source of the Amu River is the [[Pamir River]], which emerges from Lake [[Zorkul]] (once also known as Lake Victoria) in the [[Pamir Mountains]] (ancient [[Mount Imeon]]), and flows west to Qila-e Panja, where it joins the Wakhan River to form the Panj River. |
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Another claimed source of the Amu |
Another claimed source of the Amu River is an ice cave at the end of the [[Wakhjir]] valley, in the [[Wakhan Corridor]], in the [[Pamir Mountains]], near the border with Pakistan. A [[glacier]] turns into the Wakhan River and joins the Pamir River about {{convert|50|km}} downstream<ref>[http://www.mockandoneil.com/stg04r3.htm#oxus J. Mock and K. O'Neil (2004): Expedition Report]</ref>). |
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The Panj River forms the border of [[Afghanistan]] and [[Tajikistan]]. It flows west to [[Ishkashim, Afghanistan|Ishkashim]] where it turns north and then east north-west through the [[Hindu Kush]] passing the [[Tajik-Afghan Friendship Bridge]]. It subsequently forms the border of Afghanistan and [[Uzbekistan]] for about {{convert|200|km}}, passing [[Termez]] and the [[Afghanistan-Uzbekistan Friendship Bridge]]. It follows the border of Afghanistan and [[Turkmenistan]] for another {{convert|100|km}} before it flows into Turkmenistan at [[Kerki|Atamyrat]]. As the ''Amudarya'', it flows across Turkmenistan south to north, passing [[Türkmenabat]], and forms the border of Turkmenistan and [[Uzbekistan]] from [[Halkabat]]. It is then split into many waterways that used to form the [[river delta]] joining the Aral Sea, passing [[Urgench]], [[Daşoguz]] and other cities, but it does not reach what is left of the sea anymore and is lost in the desert. |
The Panj River forms the border of [[Afghanistan]] and [[Tajikistan]]. It flows west to [[Ishkashim, Afghanistan|Ishkashim]] where it turns north and then east north-west through the [[Hindu Kush]] passing the [[Tajik-Afghan Friendship Bridge]]. It subsequently forms the border of Afghanistan and [[Uzbekistan]] for about {{convert|200|km}}, passing [[Termez]] and the [[Afghanistan-Uzbekistan Friendship Bridge]]. It follows the border of Afghanistan and [[Turkmenistan]] for another {{convert|100|km}} before it flows into Turkmenistan at [[Kerki|Atamyrat]]. As the ''Amudarya'', it flows across Turkmenistan south to north, passing [[Türkmenabat]], and forms the border of Turkmenistan and [[Uzbekistan]] from [[Halkabat]]. It is then split into many waterways that used to form the [[river delta]] joining the Aral Sea, passing [[Urgench]], [[Daşoguz]] and other cities, but it does not reach what is left of the sea anymore and is lost in the desert. |
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Use of water from the Amu |
Use of water from the Amu River for [[irrigation]] has been a major contributing factor to the shrinking of the Aral Sea since the late 1950s. |
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Historical records state that in different periods, the river flowed into the [[Aral Sea]] (from the south), the [[Caspian Sea]] (from the east) or both, similar to the [[Syr |
Historical records state that in different periods, the river flowed into the [[Aral Sea]] (from the south), the [[Caspian Sea]] (from the east) or both, similar to the [[Syr River]] (Jaxartes, in [[Ancient Greek]]). |
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== See also == |
== See also == |
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{{commonscat|Amu Darya}} |
{{commonscat|Amu Darya}} |
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*[[Syr |
*[[Syr River]] |
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*[[Transoxiana]] |
*[[Transoxiana]] |
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*[[Mount Imeon]] |
*[[Mount Imeon]] |
Revision as of 06:40, 15 August 2009
Amu Darya | |
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Physical characteristics | |
Mouth | None, formerly Aral Sea |
Length | 2,400 km (1,500 mi) |
The Amu River (Tajik: дарёи Ому - Daryoi Omu, Dari: آمودریا - Âmudaryâ, Pashto: د آمو سيند - də Āmu Sind, [Amudaryo] Error: {{Lang-xx}}: text has italic markup (help), Turkmen: Amyderýa), also called Oxus River or Amudarya River, is a major river in Central Asia. It is formed by the junction of the Vakhsh and Panj rivers.
Names
![](http://upload.wikimedia.org/wikipedia/commons/thumb/a/a9/Bridge.Amu.Darya.Urgench.jpg/220px-Bridge.Amu.Darya.Urgench.jpg)
Amu is said to have come from the city of Āmul, now known as Türkmenabat. Many local people refer to the river as Jayhoun (جيحون) which was thought to be a derivative of Gihon, the biblical name for one of the four rivers of the Garden of Eden or paradise.[2] The river is also known by this name to most of the medieval Islamic writers.
In classical antiquity, the river was known as the Ōxus in Latin and Ὦξος Oxos in Greek — a clear derivative of Vakhsh — the name of the largest tributary of the Amu. It was known as جيحون - Jiːħuːn or Gihun in ancient Arabic sources. Jayhun was likely influenced by Dgihun, the traditional name given to it by the people who inhabited its surrounding region.[3]
In Vayu Purana and Matsya Purana, the Oxus is mentioned as the river Chakshu, flowing through the countries of Tusharas (Rishikas?), Lampakas, Pahlavas, Paradas and Shakas etc.
Description
![](http://upload.wikimedia.org/wikipedia/commons/thumb/8/85/Aral_map.png/200px-Aral_map.png)
The river is navigable for over 1450 km (800 miles). Its total length is 2400 km (1500 miles) and its drainage basin totals 534,739 square kilometres (206,464 sq mi) in area, providing a mean discharge of around 97.4 cubic kilometres (23.4 cu mi)[1] of water per year. All of the water comes from the high mountains in the south where annual precipitation can be over 1,000 mm (39 in). Even before large-scale irrigation began, high summer evaporation meant that not all of this discharge reached the Aral Sea - though there is some evidence the large Pamir glaciers provided enough melt water for the Aral to overflow during the thirteenth and fourteenth centuries A.D.
One source of the Amu River is the Pamir River, which emerges from Lake Zorkul (once also known as Lake Victoria) in the Pamir Mountains (ancient Mount Imeon), and flows west to Qila-e Panja, where it joins the Wakhan River to form the Panj River.
Another claimed source of the Amu River is an ice cave at the end of the Wakhjir valley, in the Wakhan Corridor, in the Pamir Mountains, near the border with Pakistan. A glacier turns into the Wakhan River and joins the Pamir River about 50 kilometres (31 mi) downstream[4]).
The Panj River forms the border of Afghanistan and Tajikistan. It flows west to Ishkashim where it turns north and then east north-west through the Hindu Kush passing the Tajik-Afghan Friendship Bridge. It subsequently forms the border of Afghanistan and Uzbekistan for about 200 kilometres (120 mi), passing Termez and the Afghanistan-Uzbekistan Friendship Bridge. It follows the border of Afghanistan and Turkmenistan for another 100 kilometres (62 mi) before it flows into Turkmenistan at Atamyrat. As the Amudarya, it flows across Turkmenistan south to north, passing Türkmenabat, and forms the border of Turkmenistan and Uzbekistan from Halkabat. It is then split into many waterways that used to form the river delta joining the Aral Sea, passing Urgench, Daşoguz and other cities, but it does not reach what is left of the sea anymore and is lost in the desert.
Use of water from the Amu River for irrigation 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 Aral Sea (from the south), the Caspian Sea (from the east) or both, similar to the Syr River (Jaxartes, in Ancient Greek).
See also
![](http://upload.wikimedia.org/wikipedia/en/thumb/4/4a/Commons-logo.svg/30px-Commons-logo.svg.png)
References
- Curzon, George Nathaniel. 1896. The Pamirs and the Source of the Oxus. Royal Geographical Society, London. Reprint: Elibron Classics Series, Adamant Media Corporation. 2005. ISBN 1-4021-5983-8 (pbk; ISBN 1-4021-3090-2 (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.
Notes
- ^ a b http://www.ce.utexas.edu/prof/mckinney/papers/aral/CentralAsiaWater-McKinney.pdf
- ^ William C. Brice. 1981. Historical Atlas of Islam (Hardcover). Leiden with support and patronage from Encyclopaedia of Islam. ISBN 90-04-06116-9.
- ^ Encyclopædia Britannica Online: Amu Darya
- ^ J. Mock and K. O'Neil (2004): Expedition Report