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Usoi Dam






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Coordinates: 38°1652N 72°3648E / 38.2810°N 72.6134°E / 38.2810; 72.6134
 

From Wikipedia, the free encyclopedia
 


This is an old revision of this page, as edited by Iain.mcclatchie (talk | contribs)at18:16, 28 August 2012 (Fix reference to UN report). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.
(diff)  Previous revision | Latest revision (diff) | Newer revision  (diff)

Usoi Dam
Usoi Dam viewed from behind. Sarez Lake is on the right, and the smaller body of water to the left is Shadau Lake. The earthen barrier separating the two lakes is not part of the dam.
CountryTajikistan
Satellite photo showing the Usoi Dam, the western end of Sarez Lake and the smaller Shadau Lake

The Usoi Dam is a natural landslide dam along the Murghab River in the Central Asian country of Tajikistan. At 567 metres (1,860 ft) high, it is the tallest dam in the world, either natural or man-made. The dam was created on February 18, 1911, when the 7.4-Ms Sarez earthquake caused a massive landslide that blocked the flow of the river.[1]

The dam is formed of approximately 2 cubic kilometres (0.48 cu mi) of rock dislodged from the steeply sloped river valley of the Murghab, which cuts from east to west through the high and rough Pamir Mountains. It is named after the village of Usoi, which was completely buried by the 1911 landslide. The dam rises to a height of 500 to 700 metres (1,600 to 2,300 ft) from the original valley floor.[2]

The basin formed by Usoi Dam now holds Sarez Lake, a 55.8-kilometre (34.7 mi)-long lake holding 16.074 cubic kilometres (13,031,000 acre⋅ft) of water. Water does not flow over the top of the dam, which would quickly cause it to erode away; instead, water seeps out of the base of the dam at a rate which approximately matches the rate of inflow, maintaining the lake at a relatively constant level. The flow averages about 45 cubic meters per second [3], and dissipates about 250 megawatts.

Geologists are concerned that the Usoi Dam may become unstable during future large-magnitude earthquakes, which are relatively common in the seismically active Pamirs, and might collapse due to liquefaction or subsequent landslides during such an event.[4] Collapse of the dam would unleash a locally catastrophic flood,[5] as the Murghab's river valley tends to be relatively narrow and steep, which would focus and maintain any flood's destructive power.

References

  1. ^ National Geophysical Data Center. "Significant Earthquake". Retrieved June 21, 2011.
  • ^ Alford, Donald; Cunha, Stephen F.; Ives, Jack D. (2000). "Lake Sarez, Pamir Mountains, Tajikistan: Mountain Hazards and Development Assistance". Mountain Research and Development. 20 (1): 20–23. JSTOR 3674203. {{cite journal}}: Unknown parameter |month= ignored (help)
  • ^ United Nations International Strategy for Disaster Reduction. "Usoi Landslide Dam and Lake Sarez: An Assessment of Hazard and Risk in the Pamir Mountains, Tajikistan" (PDF). Retrieved August 28, 2012.
  • ^ Bolt, B.A.; Horn, W.L.; Macdonald, G.A.; Scott, R.F. (1975). Geological hazards: Earthquakes, tsunamis, volcanoes, avalanches, landslides, floods. New York: Springer-Verlag. ISBN 0-387-06948-8.
  • ^ "Usoi Dam & Lake Sarez, Tajikistan: Complex Mega-Flood Hazard". Biot Reports. Suburban Emergency Management Project. October 25, 2009.
  • External links

    38°16′52N 72°36′48E / 38.2810°N 72.6134°E / 38.2810; 72.6134


    Retrieved from "https://en.wikipedia.org/w/index.php?title=Usoi_Dam&oldid=509640264"

    Categories: 
    Dams in Tajikistan
    Lakes of Tajikistan
    Gorno-Badakhshan Autonomous Province
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    Pages using gadget WikiMiniAtlas
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    This page was last edited on 28 August 2012, at 18:16 (UTC).

    This version of the page has been revised. Besides normal editing, the reason for revision may have been that this version contains factual inaccuracies, vandalism, or material not compatible with the Creative Commons Attribution-ShareAlike License.



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