Endorheic basin Totally Explained

Everything about Endorheic Basin totally explained

An endorheic basin (from Greek endo ‘inside’ + rhein ‘to flow’; also terminal or closed basin) is a closed drainage basin that retains water and allows no outflow to other bodies of water such as rivers or oceans. Normally the water accruing in drainage basins flows out through surface rivers or by underground diffusion through permeable rock to the oceans. However, in an endorheic basin, rain (or other precipitation) that falls within it doesn't flow out but may only leave the drainage system by evaporation and seepage. The bottom of such a basin is typically occupied by a salt lake or salt pan. Endorheic basins are also called internal drainage systems.
Endorheic regions, in contrast to exorheic regions which flow to the ocean in geologically defined patterns, are closed hydroloic systems. Their surface waters drain to inland terminal locations where the water evaporates or seeps into the ground, having no access to discharge into the sea. Endorheic water bodies include some of the largest lakes in the world, such as the Aral Sea and the Caspian Sea, the world’s largest saline body of water cut off from the ocean.
Endorheic lakes are usually in the interior of a body mass, far from an ocean. Their watersheds often confined by natural geologic land formations such as a mountain range, cutting off water access to the ocean. The inland water flow into dry watersheds where the water evaporates, leaving a high concentration of minerals and other inflow erosion products. Over time this input of erosion products can cause the endorheic lake to become relatively saline. Since the main outflow pathways of these lakes are chiefly through evaporation and seepage, endorheic lakes are usually more sensitive to environmental pollutants inputs than water bodies that have access to oceans.

Occurrence

Endorheic regions can occur in any climate but are most commonly found in hot desert locations. In areas where rainfall is higher, riparian erosion will generally carve drainage channels (particularly in times of flood), breaking the enclosed endorheic hydrological system’s geographical barrier and opening it to the surrounding terrain. The Black Sea was likely such a lake, having once been an independent hydrological system before the Mediterranean Sea broke through the terrain separating the two.
Endorheic regions tend to be far inland with their boundaries defined by mountains or other geological features that sever their access to oceans. Since the inflowing water can evacuate only through seepage or evaporation, dried minerals or other products collect in the basin, eventually making the water saline and also making the basin vulnerable to pollution. Approximately 18 percent of the earth’s land drains to endorheic lakes or seas, the largest of these land areas being the interior of Asia. In deserts, water inflow is low and loss to solar evaporation high, drastically reducing the formation of complete drainage systems. Closed water flow areas often lead to the concentration of salts and other minerals in the basin. Minerals leached from the surrounding rocks are deposited in the basin, and left behind when the water evaporates. Thus endorheic basins often contain extensive salt pans (also called salt flats, salt lakes, alkali flats or playas). These areas tend to be large, flat hardened surfaces and are sometimes used for aviation runways or land speed record attempts.
Both permanent and seasonal endorheic lakes can form in endorheic basins. Some endorheic basins are essentially stable, climate change having reduced precipitation to the degree that a lake no longer forms. Even most permanent endorheic lakes change size and shape dramatically over time, often becoming much smaller or breaking into several smaller parts during the dry season. As humans have expanded into previously uninhabitable desert areas, the river systems that feed many endorheic lakes have been altered by the construction of dams and aqueducts. As a result many endorheic lakes in developed or developing countries have contracted dramatically, resulting in increased salinity, higher concentrations of pollutants, and the disruption of ecosystems.

Notable endorheic basins and lakes

Antarctica

Endorheic lakes in Antarctica are located in the McMurdo Dry Valleys, Victoria Land, Antarctica, the largest ice-free area in Antarctica.

Don Juan Pond in Wright Valley is fed by groundwater from a rock glacier and remains unfrozen throughout the year.
Lake Vanda in Wright Valley has a perennial ice cover, the edges of which melt in the summer allowing flow from the longest river in Antarctica, the Onyx River. The lake is over 70 m deep and is hypersaline.
Lake Bonney is in Taylor Valley and has a perennial ice over and two lobes separated by the Bonney Riegel. The lake is fed by glacial melt and discharge from Blood Falls. Its unique glacial history has resulted in a hypersaline brine in the bottom waters and fresh water at the surface.
Lake Hoare, in Taylor Valley, is the freshest of the Dry Valley lakes receiving its melt almost exclusively from the Canada Glacier. The lake has an ice cover and forms a moat during the Austral summer.
Lake Fryxell, in adjacent to the Ross Sea in Taylor Valley. The lake has an ice cover and receives its water from numerous glacial meltwater streams for approximately 6 weeks out of the year. Its salinity increases with depth.

Asia

Much of western and Central Asia is a single, giant inland basin. It contains a number of lakes, including:

The Central Asian Internal Drainage Basin, the largest of the three major basins covering Mongolia.

The Caspian Sea, the largest lake on Earth. In fact, a large part of Eastern Europe drained by the Volga River also belongs to its basin.

The Aral Sea, whose tributary rivers have been diverted, leading to a dramatic shrinkage of the lake. The resulting ecological disaster has brought the plight faced by internal drainage basins to public attention.

Lake Balkhash (Kazakhstan)

Lop Nur Basin, in the southeastern portion of Xinjiang Uygur Autonomous Region in northwestern China

Issyk-Kul, Son-Kul and Chatyr-Kul lakes in Kyrgyzstan

Sistan Basin covering areas of Iran and Afghanistan

Tarim Basin in Xinjiang Uyghur Autonomous Region

Uvs Nuur basin, Mongolia, Tuvan Republic of Russia

The Dead Sea, the lowest surface point on Earth and one of its saltiest bodies of water, lies between Israel and Jordan.

Sambhar Lake in Rajasthan, north-western India, is also the terminal point of an endorheic basin.

Australia

Australia, being very dry and having exceedingly low runoff ratios due to its ancient soils, has a great prominence of variable, endorheic drainages. The most important are:

Lake Eyre Basin, which drains into the highly variable Lake Eyre and includes Lake Frome.

Lake Torrens, to the west of the Flinders Ranges in South Australia.

Lake Corangamite, a highly saline crater lake in western Victoria.

Lake George, formerly connected to the Murray-Darling Basin

Africa

Lake Turkana in Kenya

The Okavango Delta, an endorheic inland delta in the Kalahari Desert of Botswana

Lake Ngami in Botswana

Lake Chad (between Chad and Cameroon), fed by the Chari and Logon rivers

Etosha pan in Namibia’s Etosha National Park

Qattara Depression in Egypt

Chott Melrhir in Algeria

Lake Chilwa in Malawi

Afar Depression in Eritrea, Ethiopia and Djibouti

North America

The Valley of Mexico. In Pre-Columbian times, the Valley was substantially covered with five lakes, including Lake Texcoco, Lake Xochimilco, and Lake Chalco.

Crater Lake in Oregon

Devil's Lake (North Dakota)

Devil's Lake (Wisconsin)

The Great Divide Basin in Wyoming, a small endorheic basin that straddles the Continental Divide.

The Great Basin, which covers much of Nevada and Utah, includes:

The Black Rock Desert in Nevada, location of the Thrust2 and ThrustSSC landspeed record runs, and the annual home to the Burning Man festival
Death Valley in California and Nevada, the lowest land point in the United States
Groom Dry Lake in Nevada, location of the secret Area 51 base
Utah’s Great Salt Lake, the largest terminal lake in the Western Hemisphere
Salton Sea in California, a lake accidentally created in 1905 when irrigation canals ruptured, filling a desert endorheic basin and recreating an ancient saline sea
Utah’s Sevier Lake
Pyramid Lake in Nevada
Mono Lake in California

Rogers Lake, at Edwards Air Force Base in California

Tulare Lake, an endorheic basin at the southern end of the San Joaquin Valley fed by the Kern River; since the late 19th century the lake bed has been reclaimed and used as farmland, though it occasionally floods when rainfall is especially heavy

New Mexico has a number of desert endorheic basins including:

The Tularosa Basin, a rift valley;
Zuni Salt Lake, a maar;

Bolsón de Mapimí, in northern Mexico;

Guzmán Basin, in northern Mexico southwestern New Mexico;

Lago de Atitlán, in the highlands of Guatemala;

Europe

Neusiedlersee in Austria

Lake Trasimeno in Italy

Lake Velence in Hungary

Lake Prespa between Albania, Greece and Macedonia All these lakes are drained, however, either through manmade canals or via karstic phenomena. Minor additional endorheic lakes exist throughout the Mediterranean countries Spain (for example Laguna de Gallocanta), Italy, Cyprus (Larnaca and Akrotiri salt lakes) and Greece.

South America

Altiplano basin, one of the largest and second highest in the world.

Lake Valencia (Spanish: Lago de Valencia) the second largest lake in Venezuela.

Salar de Atacama, Atacama Desert, Chile (although close to the Altiplano it isn't part of it)

Northwest Pampas Basins in the Dry Pampas of Argentina

Southwest Pampas Basins in the Dry Pampas of Argentina

Meseta Somuncura in the Patagonia region of Argentina

Ancient

Some of the Earth’s ancient endorheic systems include:

The Black Sea, until its merger with the Mediterranean

The Mediterranean Sea itself and all its tributary basins, during its Messinian desiccation (5 m.y. BP aprox.) as it became disconnected from the Atlantic Ocean.

Lake Lahontan in the western US

Ebro and Duero basins, draining most of northern Spain during the Neogene and perhaps Pliocene.

Lake Bonneville (Utah)Further Information

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