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Water flow rate and power
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The dam is formed of approximately {{convert|2|km3|mi3}} of rock dislodged from the steeply sloped river valley of the [[Murghab River|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 {{convert|500|to|700|m|ft}} from the original valley floor.<ref>{{cite journal |last=Alford |first=Donald |last2=Cunha |first2=Stephen F. |last3=Ives |first3=Jack D. |year=2000 |month=February |title=Lake Sarez, Pamir Mountains, Tajikistan: Mountain Hazards and Development Assistance |journal=Mountain Research and Development |volume=20 |issue=1 |pages=20–23 |jstor=3674203 }}</ref> |
The dam is formed of approximately {{convert|2|km3|mi3}} of rock dislodged from the steeply sloped river valley of the [[Murghab River|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 {{convert|500|to|700|m|ft}} from the original valley floor.<ref>{{cite journal |last=Alford |first=Donald |last2=Cunha |first2=Stephen F. |last3=Ives |first3=Jack D. |year=2000 |month=February |title=Lake Sarez, Pamir Mountains, Tajikistan: Mountain Hazards and Development Assistance |journal=Mountain Research and Development |volume=20 |issue=1 |pages=20–23 |jstor=3674203 }}</ref> |
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The basin formed by Usoi Dam now holds [[Sarez Lake]], a {{convert|55.8|km|mi|adj=on}}-long lake holding {{convert|16.074|km3|acre.ft|lk=out}} 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 basin formed by Usoi Dam now holds [[Sarez Lake]], a {{convert|55.8|km|mi|adj=on}}-long lake holding {{convert|16.074|km3|acre.ft|lk=out}} 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 <ref>{{cite web |url=http://www.preventionweb.net/files/696_USOI.pdf|accessdate=August 28, 2012}}</ref>, and dissipates about 250 megawatts. |
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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.<ref>{{cite book |last=Bolt |first=B.A. |last2=Horn |first2=W.L. |last3=Macdonald |first3=G.A. |last4=Scott |first4=R.F. |title=Geological hazards: Earthquakes, tsunamis, volcanoes, avalanches, landslides, floods |year=1975 |publisher=Springer-Verlag |location=New York |isbn=0-387-06948-8}}</ref> Collapse of the dam would unleash a locally catastrophic flood,<ref>{{cite web |url=http://www.semp.us/publications/biot_reader.php?BiotID=661 |title=Usoi Dam & Lake Sarez, Tajikistan: Complex Mega-Flood Hazard |date=October 25, 2009 |work=Biot Reports |publisher=Suburban Emergency Management Project |accessdate=}}</ref> as the Murghab's river valley tends to be relatively narrow and steep, which would focus and maintain any flood's destructive power. |
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.<ref>{{cite book |last=Bolt |first=B.A. |last2=Horn |first2=W.L. |last3=Macdonald |first3=G.A. |last4=Scott |first4=R.F. |title=Geological hazards: Earthquakes, tsunamis, volcanoes, avalanches, landslides, floods |year=1975 |publisher=Springer-Verlag |location=New York |isbn=0-387-06948-8}}</ref> Collapse of the dam would unleash a locally catastrophic flood,<ref>{{cite web |url=http://www.semp.us/publications/biot_reader.php?BiotID=661 |title=Usoi Dam & Lake Sarez, Tajikistan: Complex Mega-Flood Hazard |date=October 25, 2009 |work=Biot Reports |publisher=Suburban Emergency Management Project |accessdate=}}</ref> as the Murghab's river valley tends to be relatively narrow and steep, which would focus and maintain any flood's destructive power. |
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| Usoi Dam | |
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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.
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| Country | Tajikistan |
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.
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38°16′52″N 72°36′48″E / 38.2810°N 72.6134°E / 38.2810; 72.6134
