List of drying lakes

Last updated

Satellite imagery over Iran from 1984 to 2014 revealing Lake Urmia's diminishing surface area.

A number of natural lakes throughout the world are drying or completely dry owing to irrigation or urban use diverting inflow. [1] [2]

Contents

List

List of drying lakes
Lake nameLocationCoordinatesOriginal sizeas ofReduced sizeas ofReferences
Aral Sea Kazakhstan and Uzbekistan 45°N60°E / 45°N 60°E / 45; 60 (Aral Sea) 68,000 km2 (26,000 sq mi)196014,280 km2 (5,510 sq mi)2010 [3]
Lake Chad Cameroon, Chad, Niger and Nigeria 13°00′N14°30′E / 13.0°N 14.5°E / 13.0; 14.5 (Lake Chad) 22,000 km2 (8,500 sq mi)1966300 km2 (120 sq mi)2006 [4]
Qinghai Lake China 37°00′N100°06′E / 37.0°N 100.1°E / 37.0; 100.1 (Qinghai Lake) 6,000 km2 (2,300 sq mi)4,543 km2 (1,754 sq mi)2020 [5] [6] [7]
Lake Urmia Iran 37°42′N45°24′E / 37.7°N 45.4°E / 37.7; 45.4 (Lake Urmia) 5,000 km2 (1,900 sq mi)2,820 km2 (1,090 sq mi)2021 [8]
Great Salt Lake Utah, U.S. 41°12′N112°30′W / 41.2°N 112.5°W / 41.2; -112.5 (Great Salt Lake) 4,400 km2 (1,700 sq mi)1980s2,500 km2 (950 sq mi)2021 [9] [10]
Poyang Lake Jiangxi, China 29°06′N116°18′E / 29.1°N 116.3°E / 29.1; 116.3 (Poyang Lake) 3,500 km2 (1,400 sq mi)200 km2 (77 sq mi)2012 [11]
Lake Poopó Bolivia 18°36′S67°06′W / 18.6°S 67.1°W / -18.6; -67.1 (Lake Poopó) 3,000 km2 (1,200 sq mi)02015 [12]
Lake Chany Novosibirsk Oblast, Russia 54°48′N77°30′E / 54.8°N 77.5°E / 54.8; 77.5 (Lake Chany) 2,500 km2 (970 sq mi)19701,700 km2 (660 sq mi)2024 [13]
Hamun Lake Irano-Afghan border 30°48′N61°42′E / 30.8°N 61.7°E / 30.8; 61.7 (Hamun Lake) 2,000 km2 (770 sq mi)02002 [14]
Lop Nur Xinjiang, China 40°30′N90°30′E / 40.5°N 90.5°E / 40.5; 90.5 (Lop Nur) 2,000 km2 (770 sq mi)1950s01970 [15]
Tulare Lake California, U.S. 36°00′N119°48′W / 36.0°N 119.8°W / 36.0; -119.8 (Tulare Lake) 1,800 km2 (690 sq mi)1880

5.2 km2 (2 sq mi)

2023 [16]
Lake Chapala Mexico 20°12′N103°00′W / 20.2°N 103.0°W / 20.2; -103.0 (Lake Chapala) 1,048 km2 (405 sq mi)1986812 km2 (314 sq mi)2001 [17]
Dead Sea Israel, Jordan, and Palestine 31°30′N35°30′E / 31.5°N 35.5°E / 31.5; 35.5 (Dead Sea) 1,030 km2 (400 sq mi)1960605 km2 (234 sq mi)2016 [18] [19]
Lake Ebinur Xinjiang, China 44°54′N83°00′E / 44.9°N 83°E / 44.9; 83 (Lake Ebi) 1,000 km2 (390 sq mi)1955500 km2 (190 sq mi)2014 [20] [21]
Salton Sea California, U.S. 33°18′N115°48′W / 33.3°N 115.8°W / 33.3; -115.8 (Salton Sea) 940 km2 (363 sq mi)2003832 km2 (321 sq mi)2022 [22] [23]
Lake Faguibine Mali 16°42′N4°00′W / 16.7°N 4.0°W / 16.7; -4.0 (Lake Faguibine) 590 km2 (230 sq mi)197402000 [24]
Pyramid Lake Nevada, U.S. 40°06′N119°36′W / 40.1°N 119.6°W / 40.1; -119.6 (Pyramid Lake) 510 km2 (195 sq mi) [25] [26]
Lake Amik Turkey 36°18′N36°18′E / 36.3°N 36.3°E / 36.3; 36.3 (Lake Amik) 300–350 km2 (120–140 sq mi)1950s02012 [27]
Lake Cuitzeo Michoacán, Mexico 19°56′N101°05′W / 19.93°N 101.08°W / 19.93; -101.08 (Lake Cuitzeo) 300 km2 (120 sq mi)1941 [28]
Owens Lake California, U.S. 36°26′N117°57′W / 36.43°N 117.95°W / 36.43; -117.95 (Owens Lake) 280 km2 (110 sq mi)191301926 [29]
Walker Lake Nevada, U.S. 38°41′N118°44′W / 38.69°N 118.74°W / 38.69; -118.74 (Walker Lake) 280 km2 (107 sq mi)1882130 km2 (50 sq mi)2005 [30]
Alan Nur Xinjiang, China 45°48′N85°56′E / 45.80°N 85.93°E / 45.80; 85.93 (Alan Nur) 238 km2 (92 sq mi)195001970 [31] [32]
Mono Lake California, U.S. 38°01′N119°01′W / 38.02°N 119.01°W / 38.02; -119.01 (Mono Lake) 220 km2 (86 sq mi)1941170 km2 (66 sq mi)2015 [33]
Lake Albert South Australia 35°38′S139°17′E / 35.63°S 139.28°E / -35.63; 139.28 (Lake Albert) 168 km2 (65 sq mi) [34] [35]
Lake Hindmarsh Australia 36°04′S141°55′E / 36.06°S 141.91°E / -36.06; 141.91 (Lake Hindmarsh) 135 km2 (52 sq mi)197502000 [36]
Lake Shalkar Kazakhstan 47°48′N59°35′E / 47.800°N 59.583°E / 47.800; 59.583 (Lake Shalkar) 60 km2 (23 sq mi)19007.9 km2 (3.1 sq mi)2024 [37]
Lake Hula Israel 33°06′N35°36′E / 33.1°N 35.6°E / 33.1; 35.6 14 km2 (5.4 sq mi)1940s01950s [38]

See also

Related Research Articles

<span class="mw-page-title-main">Aral Sea</span> Lake between Kazakhstan and Uzbekistan

The Aral Sea was an endorheic lake lying between Kazakhstan to its north and Uzbekistan to its south, which began shrinking in the 1960s and largely dried up by the 2010s. It was in the Aktobe and Kyzylorda regions of Kazakhstan and the Karakalpakstan autonomous region of Uzbekistan. The name roughly translates from Mongolic and Turkic languages to "Sea of Islands", a reference to the large number of islands that once dotted its waters. The Aral Sea drainage basin encompasses Uzbekistan and parts of Afghanistan, Iran, Kazakhstan, Kyrgyzstan, Tajikistan, and Turkmenistan.

<span class="mw-page-title-main">Endorheic basin</span> Closed drainage basin that has no outflow

An endorheic basin is a drainage basin that normally retains water and allows no outflow to other, external bodies of water ; instead, the water drainage flows into permanent and seasonal lakes and swamps that equilibrate through evaporation. Endorheic basins are also called closed basins, terminal basins, and internal drainage systems.

<span class="mw-page-title-main">Salton Sea</span> Shallow saline lake in southern California

The Salton Sea is a shallow, landlocked, highly saline endorheic lake in Riverside and Imperial counties at the southern end of the U.S. state of California. It lies on the San Andreas Fault within the Salton Trough, which stretches to the Gulf of California in Mexico.

<span class="mw-page-title-main">Lake Balkhash</span> Lake in southeastern Kazakhstan

Lake Balkhash, also spelt Lake Balqash, is a lake in southeastern Kazakhstan, one of the largest lakes in Asia and the 15th largest in the world. It is located in the eastern part of Central Asia and sits in the Balkhash-Alakol Basin, an endorheic (closed) basin. The basin drains seven rivers, the primary of which is the Ili, bringing most of the riparian inflow; others, such as the Karatal, bring surface and subsurface flow. The Ili is fed by precipitation, largely vernal snowmelt, from the mountains of China's Xinjiang region.

<span class="mw-page-title-main">McMurdo Dry Valleys</span> Snow-free valleys in Antarctica

The McMurdo Dry Valleys are a row of largely snow-free valleys in Antarctica, located within Victoria Land west of McMurdo Sound. The Dry Valleys experience extremely low humidity and surrounding mountains prevent the flow of ice from nearby glaciers. The rocks here are granites and gneisses, and glacial tills dot this bedrock landscape, with loose gravel covering the ground. It is one of the driest places on Earth and is sometimes claimed to have not seen rain in nearly two million years, though this is highly unlikely and several anecdotal accounts of rainfall within the Dry Valleys exist.

<span class="mw-page-title-main">Labrador Sea</span> Arm of the North Atlantic Ocean

The Labrador Sea is an arm of the North Atlantic Ocean between the Labrador Peninsula and Greenland. The sea is flanked by continental shelves to the southwest, northwest, and northeast. It connects to the north with Baffin Bay through the Davis Strait. It is a marginal sea of the Atlantic.

<span class="mw-page-title-main">Salt lake</span> Landlocked body of water which has a high concentration of salts

A salt lake or saline lake is a landlocked body of water that has a concentration of salts and other dissolved minerals significantly higher than most lakes. In some cases, salt lakes have a higher concentration of salt than sea water; such lakes can also be termed hypersaline lakes, and may also be pink lakes on account of their colour. An alkalic salt lake that has a high content of carbonate is sometimes termed a soda lake.

<span class="mw-page-title-main">Badwater Basin</span> Salt-filled basin in Death Valley National Park, containing the lowest point in North America

Badwater Basin is an endorheic basin in Death Valley National Park, Death Valley, Inyo County, California, noted as the lowest point in North America and the United States, with a depth of 282 ft (86 m) below sea level. Mount Whitney, the highest point in the contiguous United States, is only 84.6 miles (136 km) to the northwest.

<span class="mw-page-title-main">Etosha Pan</span> Big endorheic salt ville in Namibias north

The Etosha Pan is a large endorheic salt pan, forming part of the Cuvelai-Etosha Basin in the north of Namibia. It is a vast hollow in the ground in which water may collect or in which a deposit of salt remains after water has evaporated. The 120-kilometre-long (75-mile-long) dry lakebed and its surroundings are protected as Etosha National Park, Namibia's second-largest wildlife park, covering 22,270 square kilometres (8,600 sq mi). The pan is mostly dry but after heavy rains it is flooded with a thin layer of water, which is heavily salted by the mineral deposits on the surface.

<span class="mw-page-title-main">Toshka Lakes</span> Lakes in Egypt

Toshka Lakes is the name given to recently formed endorheic lakes in the Sahara Desert of Egypt. Their presence is caused by periodic overflow from Lake Nasser.

<span class="mw-page-title-main">Mar Chiquita Lake (Córdoba)</span> Salt lake located in the northeast of the province of Córdoba, in central Argentina

Mar Chiquita or Mar de Ansenuza is an endorheic salt lake located in the northeast of the province of Córdoba, in central Argentina. The northeast corner of the lake also extends into southeastern Santiago del Estero Province. It is the largest of the naturally occurring saline lakes in Argentina. The lake is located in parts of five departments in the two provinces.

<span class="mw-page-title-main">South Aral Sea</span> Dried lake

The South Aral Sea was a lake in the basin of the former Aral Sea which formed in 1987 when that body divided in two, due to diversion of river inflow for agriculture. In 2003, the South Aral Sea itself split into eastern and western basins, the Eastern Sea and the West Aral Sea, connected by a narrow channel that balanced surface levels but did not allow mixing, and in 2005 the North Aral Sea was dammed to prevent the collapse of its fisheries, cutting off the only remaining inflow to the southern lakes. In 2008, the Eastern Sea split again, and in May 2009 had almost completely dried out, leaving only the small permanent Barsakelmes Lake between the Northern and Western Seas and increasing the expanse of the Aralkum desert. In 2010, it was partially filled again by meltwater, and by 2014 was once again dry. The West Aral Sea has some replenishment from groundwater in the northwest.

<span class="mw-page-title-main">Sonny Bono Salton Sea National Wildlife Refuge</span> Protected area in Imperial Valley, California

The Sonny Bono Salton Sea National Wildlife Refuge is located in the Imperial Valley of California, 40 miles (64 km) north of the Mexican border. Situated at the southern end of the Salton Sea, the refuge protects one of the most important nesting sites and stopovers along the Pacific Flyway. Despite its location in the Colorado Desert, a subdivision of the larger Sonoran Desert, the refuge contains marine, freshwater, wetland, and agricultural habitats which provide sanctuary for hundreds of birds and wetland species, including several that have been listed as endangered or sensitive by the U.S. Fish and Wildlife Service.

<span class="mw-page-title-main">Murray Darling Depression</span>

The Murray Darling Depression , also known as the Murray-Darling woodlands and mallee, is a 19,717,651 HA biogeographic region and an ecoregion in southeastern Australia consisting of a wooded plain through which flow two of Australia's biggest rivers, the Murray and the Darling. There are several modern human settlements in the bioregion including Ivanhoe and Manilla, but the region also contains some of the oldest known human occupation sites in Australia.

The Kızılırmak Delta is the delta of the Kızılırmak River where it flows into the Black Sea, 40 km east of the city of Samsun. The delta is the third largest in Turkey and has the biggest wetland in Turkey's Black Sea Region. The wetland is a key biodiversity area and one of several internationally important Ramsar sites in Turkey because of its rich bird and plant life. There is a bird reserve which is important for migration.

The Salton Buttes are a group of volcanoes in Southern California, on the Salton Sea. They consist of a 7-kilometer (4.3 mi)-long row of five lava domes, named Mullet Island, North Red Hill, Obsidian Butte, Rock Hill and South Red Hill. They are closely associated with a fumarolic field and a geothermal field, and there is evidence of buried volcanoes underground. In pre-modern times Obsidian Butte was an important regional source of obsidian.

References

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