Lake Van | |
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From space, September 1996
(top of image is roughly northwest) |
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Coordinates | 38°38′N 42°49′E / 38.633°N 42.817°ECoordinates: 38°38′N 42°49′E / 38.633°N 42.817°E |
Type | saline lake |
Primary inflows | Karasu, Hoşap, Güzelsu, Bendimahi, Zilan and Yeniköprü streams |
Primary outflows | none |
Catchment area | 12,500 km2 (4,800 sq mi) |
Basin countries | Turkey |
Max. length | 119 km (74 mi) |
Surface area | 3,755 km2 (1,450 sq mi) |
Average depth | 171 m (561 ft) |
Max. depth | 451 m (1,480 ft) |
Water volume | 607 km3 (146 cu mi) |
Shore length1 | 430 km (270 mi) |
Surface elevation | 1,640 m (5,380 ft) |
Islands | Akdamar, Çarpanak (Ktuts), Adır (Lim), Kuş (Arter) |
Settlements | Van, Tatvan, Ahlat, Erciş |
1 Shore length is not a well-defined measure. |
Lake Van (Turkish: Van Gölü, Armenian: Վանա լիճ, Vana lič̣, Kurdish: Gola Wanê), the largest lake in Turkey, lies in the far east of that country in the provinces of Van and Bitlis. It is a saline soda lake, receiving water from numerous small streams that descend from the surrounding mountains. Lake Van is one of the world's largest endorheic lakes (having no outlet) - a volcanic eruption blocked the original outlet from the basin in ancient times. Although Lake Van has an altitude of 1,640 m (5,380 ft) in a region with harsh winters, its high salinity prevents most of it from freezing, and even the shallow northern section freezes only rarely.
Lake Van is 119 kilometres (74 mi) across at its widest point, averaging a depth of 171 metres (561 ft) with a maximum recorded depth of 451 metres (1,480 ft). The lake surface lies 1,640 metres (5,380 ft) above sea level and the shore length is 430 kilometres (270 mi). Lake Van has an area of 3,755 km2 (1,450 sq mi) and a volume of 607 cubic kilometres (146 cu mi).
The western portion of the lake is deepest, with a large basin deeper than 400 m (1,300 ft) lying northeast of Tatvan and south of Ahlat. The eastern arms of the lake are shallower. The Van-Ahtamar portion shelves gradually, with a maximum depth of about 250 m (820 ft) on its northwest side where it joins the rest of the lake. The Erciş arm is much shallower, mostly less than 50 m (160 ft), with a maximum depth of about 150 m (490 ft).
The lake water is strongly alkaline (pH 9.7–9.8) and rich in sodium carbonate and other salts, which are extracted by evaporation and used as detergents.
The lake's outlet was blocked at some time during the , when lava flows from Nemrut volcano blocked westward outflow towards the Muş Plain. Now dormant, Nemrut Dağı is close to the western shore of the lake, and another dormant stratovolcano, Süphan Dağı dominates the northern side of the lake.