Sarez Lake

Coordinates: 38°12′06″N 72°45′27″E / 38.20167°N 72.75750°E / 38.20167; 72.75750
Source: Wikipedia, the free encyclopedia.
Sarez Lake
Murghab River
Basin countriesTajikistan
Max. length75.8 kilometres (47.1 mi)
Max. width3.3 kilometres (2.1 mi)
Surface area79.7 square kilometres (30.8 sq mi)
Average depth201.8 metres (662 ft)
Max. depth505 metres (1,657 ft)
Water volume16.074 cubic kilometres (3.856 cu mi)
Shore length1162 kilometres (101 mi)
Surface elevation3,263 metres (10,705 ft)
1 Shore length is not a well-defined measure.
Satellite photo of the western end of Sarez Lake showing the Usoi Dam and the smaller Shadau Lake

Sarez Lake (

romanized: Sarez Kūl) is a lake in Rushon District of Gorno-Badakhshan province, Tajikistan
. Length about 75.8 kilometres (47.1 mi), depth few hundred meters, water surface elevation about 3,263 metres (10,705 ft) above sea level and volume of water is more than 16 cubic kilometres (3.8 cu mi). The mountains around rise more than 2,300 metres (7,500 ft) above the lake level.

The lake formed in 1911, after a great

Murghab River was blocked by a big landslide. Scientists believe that the landslide dam formed by the earthquake, known as the Usoi Dam, is unstable given local seismicity, and that the terrain below the lake is in danger of catastrophic flood if the dam were to fail during a future earthquake.[1] The Usoi Dam wall survived a localised 7.2 magnitude earthquake, the 2015 Tajikistan earthquake
, on the 7th December 2015 with no visible signs of deterioration.

Shadau Lake is a small water body southwest of the Usoi Dam and west of Sarez Lake.[2]

Formation

The formation of Sarez Lake is described in the book by Middleton and Thomas:[3]

The

Murghab and Khorog
.

In 1968 a landslide caused two-meter-high waves in the lake. A 1997 conference in Dushanbe concluded that the dam was unstable and might collapse if there were another powerful earthquake. A 2004 study by the World Bank held that the dam was stable. The principal danger seems to be a partially detached mass of rock of about 3 cubic kilometres that could break loose and fall into the lake. Since the valley below the dam is so narrow, any flood would be very destructive. The result of a global risk analysis carried out by STUCKY for the World Bank was presented at the 2002 IAHR Symposium in St Petersburg [1] and at the 2006 International Congress on Large Dams [2] in Barcelona.

References

  1. ISBN 0-387-06948-8
  2. ^ "Shadau Lake on 1:110'000 map" (JPG).
  3. ISBN 978-962-217-773-4

External links
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