Aral Sea - wikipedia Aral Sea Aral Sea Aral teńizi ( Kazakh ) Orol dengizi ( Uzbek ) Аральское море ( Russian ) The Aral Sea in 1989 ( left ) and 2014 ( right ) Location Kazakhstan - Uzbekistan, Central Asia Coordinates 45 ° N 60 ° E ﻿ / ﻿ 45 ° N 60 ° E ﻿ / 45 ; 60 Coordinates : 45 ° N 60 ° E ﻿ / ﻿ 45 ° N 60 ° E ﻿ / 45 ; 60 Type endorheic, natural lake, reservoir ( North ) Primary inflows North : Syr Darya South : groundwater only ( previously the Amu Darya ) Catchment area 1,549,000 km ( 598,100 sq mi ) Basin countries Kazakhstan, Kyrgyzstan, Tajikistan, Turkmenistan, Uzbekistan, Russia, Iran Surface area 68,000 km ( 26,300 sq mi ) ( 1960, one lake ) 28,687 km ( 11,076 sq mi ) ( 1998, two lakes ) 17,160 km ( 6,626 sq mi ) ( 2004, four lakes ) North : 3,300 km ( 1,270 sq mi ) ( 2008 ) South : 3,500 km ( 1,350 sq mi ) ( 2005 ) Average depth North : 8.7 m ( 29 ft ) ( 2014 ) South : 14 -- 15 m ( 46 -- 49 ft ) ( 2005 ) Max. depth North : 42 m ( 138 ft ) ( 2008 ) 30 m ( 98 ft ) ( 2003 ) South : 37 -- 40 m ( 121 -- 131 ft ) ( 2005 ) 102 m ( 335 ft ) ( 1989 ) Water volume North : 27 km ( 6 cu mi ) ( 2007 ) Surface elevation North : 42 m ( 138 ft ) ( 2011 ) South : 29 m ( 95 ft ) ( 2007 ) 53.4 m ( 175 ft ) ( 1960 ) Settlements Aral, Kazakhstan and Mo'ynoq, Uzbekistan The map of ' Aral ' Sea of 1853 published for the Journal of the Royal Geographical Society in London Map : Location of Aral Sea ( shoreline c. 2008 ) in relation to nearby countries - Amu Darya basin in orange, Syr Darya basin in yellow The Aral Sea ( / ˈærəl / ) was an endorheic lake ( one with no outflow ) lying between Kazakhstan ( Aktobe and Kyzylorda Regions ) in the north and Uzbekistan ( Karakalpakstan autonomous region ) in the south. The name roughly translates as `` Sea of Islands '', referring to over 1,100 islands that had dotted its waters ; in the Turkic languages aral means `` island, archipelago ''. The Aral Sea drainage basin encompasses Uzbekistan and parts of Tajikistan, Turkmenistan, Kyrgyzstan, Kazakhstan, Afghanistan and Iran. Formerly one of the four largest lakes in the world with an area of 68,000 km ( 26,300 sq mi ), the Aral Sea has been shrinking since the 1960s after the rivers that fed it were diverted by Soviet irrigation projects. By 1997, it had declined to 10 % of its original size, splitting into four lakes -- the North Aral Sea, the eastern and western basins of the once far larger South Aral Sea, and one smaller intermediate lake. By 2009, the southeastern lake had disappeared and the southwestern lake had retreated to a thin strip at the western edge of the former southern sea ; in subsequent years, occasional water flows have led to the southeastern lake sometimes being replenished to a small degree. Satellite images taken by NASA in August 2014 revealed that for the first time in modern history the eastern basin of the Aral Sea had completely dried up. The eastern basin is now called the Aralkum Desert. In an ongoing effort in Kazakhstan to save and replenish the North Aral Sea, a dam project was completed in 2005 ; in 2008, the water level in this lake had risen by 12 m ( 39 ft ) compared to 2003. Salinity has dropped, and fish are again found in sufficient numbers for some fishing to be viable. The maximum depth of the North Aral Sea is 42 m ( 138 ft ) ( as of 2008 ). The shrinking of the Aral Sea has been called `` one of the planet 's worst environmental disasters ''. The region 's once - prosperous fishing industry has been essentially destroyed, bringing unemployment and economic hardship. The water from the diverted Syr Darya river is used to irrigate about 5 million acres ( 2 million hectares ) of farmland in the Ferghana Valley. The Aral Sea region is also heavily polluted, with consequential serious public health problems. UNESCO added the historical documents concerning the development of the Aral Sea to its Memory of the World Register as a unique resource to study this `` environmental tragedy ''. Contents 1 Formation 2 History 2.1 Naval history 2.2 Irrigation canals 3 Impact on environment, economy, and public health 4 Solution 4.1 Possible environmental solutions 4.2 Aral Sea Basin program 4.2. 1 ASBP : Phase One 4.2. 2 ASBP : Phase Two 4.2. 3 ASBP : Phase Three 4.3 North Aral Sea restoration work 4.4 Future of South Aral Sea 5 Institutional bodies 6 Vozrozhdeniya 7 Oil and gas exploration 8 Films 9 See also 10 References 11 Further reading 12 External links Formation Geographer Nick Middleton believes that the Amu Darya did not flow into the shallow depression that now forms the Aral Sea until the beginning of the Holocene, and it is known that the Amu Darya flowed into the Caspian Sea via the Uzboy channel until the Holocene. The Syr Darya formed a large lake in the Kyzyl Kum during the Pliocene known as the Mynbulak depression. History Most of the area around the Aral Sea was inhabited by desert nomads who left few written records. However, the Oxus delta to the south has a long history under the name of Khwarezm. It was once the westernmost border of Tang dynasty China. Naval history First Russian boats on the Aral Sea, sketch by Taras Shevchenko, 1848 Ships of Imperial Russian Navy 's Aral Flotilla in the 1850s Russian naval presence on the Aral Sea started in 1847, with the founding of Raimsk, which was soon renamed Fort Aralsk, near the mouth of the Syr Darya. Soon, the Imperial Russian Navy started deploying its vessels on the sea. Owing to the Aral Sea basin not being connected to other bodies of water, the vessels had to be disassembled in Orenburg on the Ural River, shipped overland to Aralsk ( presumably by a camel caravan ), and then reassembled. The first two ships, assembled in 1847, were the two - masted schooners named Nikolai and Mikhail. The former was a warship ; the latter was a merchant vessel meant to serve the establishment of the fisheries on the great lake. In 1848, these two vessels surveyed the northern part of the sea. In the same year, a larger warship, the Constantine, was assembled. Commanded by Lt. Alexey Butakov ( Алексей Бутаков ), the Constantine completed the survey of the entire Aral Sea over the next two years. The exiled Ukrainian poet and painter Taras Shevchenko participated in the expedition, and painted a number of sketches of the Aral Sea coast. For the navigation season of 1851, two newly built steamers arrived from Sweden, again by caravan from Orenburg. As the geological surveys had found no coal deposits in the area, the Military Governor - General of Orenburg Vasily Perovsky ordered `` as large as possible supply '' of saxaul ( Haloxylon ammodendron, a desert shrub, akin to the creosote bush ) to be collected in Aralsk for use by the new steamers. Unfortunately, saxaul wood did not turn out a very suitable fuel, and in the later years, the Aral Flotilla was provisioned, at substantial cost, by coal from the Donbass. ( This was part of the Russian conquest of Turkestan. ) Irrigation canals Further information : Great Plan for the Transformation of Nature Play media Satellite images show the changing water levels in the Aral Sea from 2000 to 2011. Timeline of shrinking In the early 1960s, the Soviet government decided the two rivers that fed the Aral Sea, the Amu Darya in the south and the Syr Darya in the east, would be diverted to irrigate the desert, in an attempt to grow rice, melons, cereals, and cotton. This was part of the Soviet plan for cotton, or `` white gold '', to become a major export. This temporarily succeeded, and in 1988, Uzbekistan was the world 's largest exporter of cotton. The construction of irrigation canals began on a large scale in the 1940s. Many of the canals were poorly built, allowing water to leak or evaporate. From the Qaraqum Canal, the largest in Central Asia, perhaps 30 to 75 % of the water went to waste. Today, only 12 % of Uzbekistan 's irrigation canal length is waterproofed. Of the 47,750 km of interfarm irrigation channels in the basin, only 28 % have anti-infiltration linings. Only 77 % of farm intakes have flow gauges, and of the 268,500 km of onfarm channels, only 21 % have anti-infiltration linings, which retain on average 15 % more water than unlined channels. By 1960, between 20 and 60 km ( 4.8 and 14.4 cu mi ) of water each year was going to the land instead of the sea. Most of the sea 's water supply had been diverted, and in the 1960s, the Aral Sea began to shrink. From 1961 to 1970, the Aral 's level fell at an average of 20 cm ( 7.9 in ) a year ; in the 1970s, the average rate nearly tripled to 50 -- 60 cm ( 20 -- 24 in ) per year, and by the 1980s, it continued to drop, now with a mean of 80 -- 90 cm ( 31 -- 35 in ) each year. The rate of water use for irrigation continued to increase ; the amount of water taken from the rivers doubled between 1960 and 2000, and cotton production nearly doubled in the same period. The disappearance of the lake was no surprise to the Soviets ; they expected it to happen long before. As early as 1964, Aleksandr Asarin at the Hydroproject Institute pointed out that the lake was doomed, explaining, `` It was part of the five - year plans, approved by the council of ministers and the Politburo. Nobody on a lower level would dare to say a word contradicting those plans, even if it was the fate of the Aral Sea. '' The reaction to the predictions varied. Some Soviet experts apparently considered the Aral to be `` nature 's error '', and a Soviet engineer said in 1968, `` it is obvious to everyone that the evaporation of the Aral Sea is inevitable. '' On the other hand, starting in the 1960s, a large - scale project was proposed to redirect part of the flow of the rivers of the Ob basin to Central Asia over a gigantic canal system. Refilling of the Aral Sea was considered as one of the project 's main goals. However, due to its staggering costs and the negative public opinion in Russia proper, the federal authorities abandoned the project by 1986. From 1960 to 1998, the sea 's surface area shrank by about 60 %, and its volume by 80 %. In 1960, the Aral Sea had been the world 's fourth - largest lake, with an area around 68,000 km ( 26,000 sq mi ) and a volume of 1,100 km ( 260 cu mi ) ; by 1998, it had dropped to 28,687 km ( 11,076 sq mi ) and eighth largest. The salinity of the Aral Sea also increased : by 1990 it was around 376 g / L. ( By comparison, the salinity of ordinary seawater is typically around 35 g / L ; the Dead Sea 's salinity varies between 300 and 350 g / L. ) In 1987, the continuing shrinkage split the lake into two separate bodies of water, the North Aral Sea ( the Lesser Sea, or Small Aral Sea ) and the South Aral Sea ( the Greater Sea, or Large Aral Sea ). In June 1991, Uzbekistan gained independence from the Soviet Union. Craig Murray, a UK ambassador to Uzbekistan in 2002, described the independence as a way for Islam Karimov to consolidate his power rather than a move away from a Soviet - style economy and its philosophy of exploitation of the land. Murray attributes the shrinkage of the Aral Sea in the 1990s to Karimov 's cotton policy. The government maintained an enormous irrigation system which Murray described as massively wasteful, with most of the water being lost through evaporation before reaching the cotton. Crop rotation was not used, and the depleted soil and monoculture required massive quantities of pesticides and fertilizer. The runoff from the fields washed these chemicals into the shrinking sea, creating severe pollution and health problems. As the water supply of the Aral Sea decreased, the demand for cotton increased and the government reacted by pouring more pesticides and fertilizer onto the land. Murray compared the system to the slavery system in the pre-Civil War United States ; forced labor was used, and profits were siphoned off by the powerful and well - connected. By summer 2003, the South Aral Sea was vanishing faster than predicted. In the deepest parts of the sea, the bottom waters were saltier than the top, and not mixing. Thus, only the top of the sea was heated in the summer, and it evaporated faster than would otherwise be expected. In 2003, the South Aral further divided into eastern and western basins. In 2004, the Aral Sea 's surface area was only 17,160 km ( 6,630 sq mi ), 25 % of its original size, and a nearly five-fold increase in salinity had killed most of its natural flora and fauna. By 2007, the sea 's area had further shrunk to 10 % of its original size. The decline of the North Aral has now been partially reversed following construction of a dam ( see below ), but the remnants of the South Aral continue to disappear and its drastic shrinkage has created the Aralkum, a desert on the former lake bed. The inflow of groundwater into the South Aral Sea will probably not in itself be able to stop the desiccation, especially without a change in irrigation practices. This inflow of about 4 km ( 0.96 cu mi ) per year is larger than previously estimated. The groundwater originates in the Pamirs and Tian Shan Mountains and finds its way through geological layers to a fracture zone at the bottom of the Aral. The Aral Sea from space, North at bottom, August 1985 The Aral Sea from space, North at bottom, August 1997 The Aral Sea from space, North at top, August 2009 The Aral Sea from space, North at top, August 2017 Impact on environment, economy, and public health The ecosystems of the Aral Sea and the river deltas feeding into it have been nearly destroyed, not least because of the much higher salinity. The receding sea has left huge plains covered with salt and toxic chemicals resulting from weapons testing, industrial projects, and pesticides and fertilizer runoff. These substances form wind - borne toxic dust that spreads throughout the region. As a result, the land around the Aral Sea is heavily polluted, and the people living in the area are suffering from a lack of fresh water and health problems, including high rates of certain forms of cancer and lung diseases. Respiratory illnesses, including tuberculosis ( most of which is drug resistant ) and cancer, digestive disorders, anaemia, and infectious diseases are common ailments in the region. Liver, kidney, and eye problems can also be attributed to the toxic dust storms. All of this has resulted in an unusually high fatality rate among vulnerable parts of the population : the child mortality rate is 75 in every 1,000 newborns, and maternity death is 12 in every 1,000 women. The dust storms also contribute to water shortages through salt deposition. The overuse of pesticides on crops to preserve yields has made this worse, with pesticide use far beyond health limits. Crops in the region are destroyed by salt being deposited onto the land, and fields are being flushed with water at least four times per day to try to remove the salinity from the soils. The dust storms make regional winters colder, and summers hotter. The Aral Sea fishing industry, which in its heyday employed some 40,000 and reportedly produced one - sixth of the Soviet Union 's entire fish catch, has been devastated, and former fishing towns along the original shores have become ship graveyards. Aral, originally the main fishing port, is now several miles from the sea and has seen its population decline dramatically since the beginning of the crisis. The town of Moynaq in Uzbekistan had a thriving harbor and fishing industry that employed about 30,000 people ; now it lies miles from the shore. Fishing boats lie scattered on the dry land that was once covered by water ; many have been there for 20 years. Also destroyed is the muskrat - trapping industry in the deltas of the Amu Darya and Syr Darya, which used to yield as many as 500,000 pelts a year. Aral Sea dust storm, March 2010 Abandoned ship near Aral, Kazakhstan A former harbor in the city of Aral Local Kazakh fisherman harvesting the day 's catch Solution Possible environmental solutions Many different solutions to the problems have been suggested over the years, varying in feasibility and cost, including : Improving the quality of irrigation canals Installing desalination plants Charging farmers to use the water from the rivers Using alternative cotton species that require less water Promoting non-agricultural economic development in upstream countries Using fewer chemicals on the cotton Cultivating crops other than cotton Installing dams to fill the Aral Sea Redirecting water from the Volga, Ob and Irtysh rivers to restore the Aral Sea to its former size in 20 -- 30 years at a cost of US $30 -- 50 billion Pumping sea water into the Aral Sea from the Caspian Sea via a pipeline, and diluting it with fresh water from local catchment areas In January 1994, Kazakhstan, Uzbekistan, Turkmenistan, Tajikistan, and Kyrgyzstan signed a deal to pledge 1 % of their budgets to help the sea recover. In March 2000, UNESCO presented their `` Water - related vision for the Aral Sea basin for the year 2025 '' at the second World Water Forum in The Hague. This document was criticized for setting unrealistic goals and for giving insufficient attention to the interests of the area immediately around the former lakesite, implicitly giving up on the Aral Sea and the people living on the Uzbek side of the lake. By 2006, the World Bank 's restoration projects, especially in the North Aral, were giving rise to some unexpected, tentative relief in what had been an extremely pessimistic picture. Aral Sea basin program The future of the Aral Sea and the responsibility for its survival are now in the hands of the five countries : Kazakhstan, Uzbekistan, Tajikistan, Kyrgyzstan, and Turkmenistan. In 1994, they adopted the Aral Sea Basin Program. The Program 's four objectives are : To stabilize the environment of the Aral Sea Basin To rehabilitate the disaster area around the sea To improve the management of the international waters of the Aral Sea Basin To build the capacity of institutions at the regional and national level to advance the program 's aims Asbp : phase one The first phase of the plan effectively began with the first involvement from the World Bank in 1992, and was in operation until 1997. It was ineffectual for a number of reasons, but mainly because it was focused on improving directly the land around the Aral Sea, whilst not intervening in the water usage upstream. There was considerable concern amongst the Central Asian governments, which realised the importance of the Aral Sea in the ecosystem and the economy of Central Asia, and they were prepared to cooperate, but they found it difficult to implement the procedures of the plan. This is due in part to a lack of co-operation among the affected people. The water flowing into the Aral Sea has long been considered an important commodity, and trade agreements have been made to supply the downstream communities with water in the spring and summer months for irrigation. In return, they supply the upstream countries with fuel during the winter, instead of storing water during the warm months for hydroelectric purposes in winter. However, very few legal obligations are binding these contracts, particularly on an international stage. Asbp : phase two Phase Two of the Aral Sea Basin program followed in 1998 and ran for five years. The main shortcomings of phase two were due to its lack of integration with the local communities involved. The scheme was drawn up by the World Bank, government representatives, and various technical experts, without consulting those who would be affected. An example of this was the public awareness initiatives, which were seen as propagandist attempts by people with little care or understanding of their situation. These failures have led to the introduction of a new plan, funded by a number of institutions, including the five countries involved and the World Bank. Asbp : phase three In 1997, a new plan was conceived which would continue with the previous restoration efforts of the Aral Sea. The main aims of this phase are to improve the irrigation systems currently in place, whilst targeting water management at a local level. The largest project in this phase is the North Aral Sea Project, a direct effort to recover the northern region of the Aral Sea. The North Aral Sea Project 's main initiative is the construction of a dam across the Berg Strait, a deep channel which connects the North Aral Sea to the South Aral Sea. The Kok - Aral Dam is eight miles long and has capacity for over 29 cubic kilometres of water to be stored in the North Aral Sea, whilst allowing excess to overflow into the South Aral Sea. North Aral Sea restoration work Comparison of the North Aral Sea before ( below ) and after ( above ) the construction of Dike Kokaral completed in 2005. Comparison of the North Aral Sea in 2000 and 2011. Work is being done to restore in part the North Aral Sea. Irrigation works on the Syr Darya have been repaired and improved to increase its water flow, and in October 2003, the Kazakh government announced a plan to build Dike Kokaral, a concrete dam separating the two halves of the Aral Sea. Work on this dam was completed in August 2005 ; since then, the water level of the North Aral has risen, and its salinity has decreased. As of 2006, some recovery of sea level has been recorded, sooner than expected. `` The dam has caused the small Aral 's sea level to rise swiftly to 38 m ( 125 ft ), from a low of less than 30 m ( 98 ft ), with 42 m ( 138 ft ) considered the level of viability. '' Economically significant stocks of fish have returned, and observers who had written off the North Aral Sea as an environmental disaster were surprised by unexpected reports that, in 2006, its returning waters were already partly reviving the fishing industry and producing catches for export as far as Ukraine. The restoration reportedly gave rise to long - absent rain clouds and possible microclimate changes, bringing tentative hope to an agricultural sector swallowed by a regional dustbowl, and some expansion of the shrunken sea. `` The sea, which had receded almost 100 km ( 62 mi ) south of the port - city of Aralsk, is now a mere 25 km ( 16 mi ) away. '' The Kazakh Foreign Ministry stated that `` The North Aral Sea 's surface increased from 2,550 square kilometers ( 980 sq mi ) in 2003 to 3,300 square kilometers ( 1,300 sq mi ) in 2008. The sea 's depth increased from 30 meters ( 98 ft ) in 2003 to 42 meters ( 138 ft ) in 2008. '' Now, a second dam is to be built based on a World Bank loan to Kazakhstan, with the start of construction initially slated for 2009 and postponed to 2011, to further expand the shrunken Northern Aral, eventually reducing the distance to Aralsk to only 6 km ( 3.7 mi ). Then, it was planned to build a canal spanning the last 6 km, to reconnect the withered former port of Aralsk to the sea. Future of South Aral Sea The Aral Sea in August 2010, with part of the eastern basin reflooded from heavy snowmelt. The Aral Sea completely loses Its Eastern Lobe in August 2014 The South Aral Sea, half of which lies in Uzbekistan, was largely abandoned to its fate. Only excess water from the North Aral Sea is now periodically allowed to flow into the largely dried - up South Aral Sea through a sluice in the dike. Discussions had been held on recreating a channel between the somewhat improved North and the desiccated South, along with uncertain wetland restoration plans throughout the region, but political will is lacking. Uzbekistan shows no interest in abandoning the Amu Darya river as an abundant source of cotton irrigation, and instead is moving toward oil exploration in the drying South Aral seabed. Attempts to mitigate the effects of desertification include planting vegetation in the newly exposed seabed ; however, intermittent flooding of the eastern basin is likely to prove problematic for any development. Redirecting what little flow there is from the Amu Darya to the western basin may salvage fisheries there while relieving the flooding of the eastern basin. Institutional bodies The Interstate Commission for Water Coordination of Central Asia ( ICWC ) was formed on February 18, 1992 to formally unite the five Central Asian countries in the hopes of solving environmental as well as socioeconomic problems in the Aral Sea region. These five states are the Republic of Kazakhstan, the Kyrgyz Republic, the Republic of Tajikistan, Turkmenistan and the Republic of Uzbekistan. The River Basin Organizations ( the BVOs ) of the Syr Darya and Amu Darya rivers were institutions called upon by the ICWC to help manage water resources. According to the ICWC, the main objectives of the body are : River basin management Water allocation without conflict Organization of water conservation on transboundary water courses Interaction with hydrometeorological services of the countries on flow forecast and account Introduction of automation into head structures Regular work on ICWC and its bodies ' activity advancement Interstate agreements preparation International relations Scientific research Training The International Fund for Saving the Aral Sea ( no ) ( IFAS ) was developed on March 23, 1993 by the ICWC to raise funds for the projects under Aral Sea Basin programs. The IFAS was meant to finance programs to save the sea and improve on environmental issues associated with the basin 's drying. This program has had some success with joint summits of the countries involved and finding funding from the World Bank to implement projects ; however, it faces many challenges, such as enforcement and slowing progress. Vozrozhdeniya Main article : Vozrozhdeniya Island `` Rebirth '' Island joins the mainland in mid-2001. Vozrozhdeniya, also known as `` Rebirth Island '', is a former island of the Aral Sea or South Aral Sea. Due to the ongoing shrinkage of the Aral, it became first a peninsula in mid-2001 and finally part of the mainland. Other islands like Kokaral and Barsa - Kelmes shared a similar fate. Since the disappearance of the Southeast Aral in 2008, Vozrozhdeniya effectively no longer exists as a distinct geographical feature. The area is now shared by Kazakhstan and Uzbekistan. In 1948, a top - secret Soviet bioweapons laboratory was established on the island, in the center of the Aral Sea which is now disputed territory between Kazakhstan and Uzbekistan. The exact history, functions and current status of this facility are still unclear, but bio-agents tested there included Bacillus anthracis, Coxiella burnetii, Francisella tularensis, Brucella suis, Rickettsia prowazekii, Variola major ( smallpox ), Yersinia pestis, botulinum toxin, and Venezuelan equine encephalitis virus. In 1971, weaponized smallpox from the island reached a nearby ship, which then allowed the virus to spread to the city of Aral. Ten people there were infected, of whom 3 died, and a massive vaccination effort involving 50,000 inhabitants ensued ( see Aral smallpox incident ). The bioweapons base was abandoned in 1992 following the disintegration of the Soviet Union the previous year. Scientific expeditions proved this had been a site for production, testing and later dumping of pathogenic weapons. In 2002, through a project organized by the United States and with Uzbekistan 's assistance, 10 anthrax burial sites were decontaminated. According to the Kazakh Scientific Center for Quarantine and Zoonotic Infections, all burial sites of anthrax were decontaminated. Oil and gas exploration Ergash Shaismatov, the deputy prime minister of Uzbekistan, announced on August 30, 2006, that the Uzbek government and an international consortium consisting of state - run Uzbekneftegaz, LUKoil Overseas, Petronas, Korea National Oil Corporation, and China National Petroleum Corporation signed a production - sharing agreement to explore and develop oil and gas fields in the Aral Sea, saying, `` The Aral Sea is largely unknown, but it holds a lot of promise in terms of finding oil and gas. There is risk, of course, but we believe in the success of this unique project. '' The consortium was created in September 2005. As of June 1, 2010, 500,000 cubic meters of gas had been extracted from the region at a depth of 3 km. Films The plight of the Aral coast was portrayed in the 1989 film Psy ( `` Dogs '' ) by Soviet director Dmitri Svetozarov. The film was shot on location in an actual ghost town located near the Aral Sea, showing scenes of abandoned buildings and scattered vessels. In 2000, the MirrorMundo foundation produced a documentary film called Delta Blues about the problems arising from the drying up of the sea. In June 2007, BBC World broadcast a documentary called Back From the Brink ? made by Borna Alikhani and Guy Creasey that showed some of the changes in the region since the introduction of the Aklak Dam. Bakhtyar Khudojnazarov 's 2012 movie Waiting for the Sea deals with the impacts on people 's life in a fishing town at the shore of the Aral Sea. In October 2013, Al Jazeera produced a documentary film called People of The Lake, directed by Ensar Altay, describing the current situation. In 2014, director Po Powell shot much of the footage for the Pink Floyd single `` Louder than Words '' video near the remains of the Aral Sea on the border between Kazakhstan and Uzbekistan. See also List of drying lakes Dead Sea Draining of the Mesopotamian marshes -- a similar water diversion project in Iraq Lake Chad Salton Sea Sistan Basin -- a large wetland ecosystem in Afghanistan and Iran on the verge of collapse Sudd -- a large marshland in Africa, site of another planned large - scale draining project Tulare Lake - California 's largest lake, drained between 1880 - 1970 References ^ Jump up to : `` DRAINAGE BASIN OF THE ARAL SEA AND OTHER TRANSBOUNDARY SURFACE WATERS IN CENTRAL ASIA '' ( PDF ). United Nations Economic Commission for Europe ( UNECE ). 2005. Retrieved 4 Feb 2016. ^ Jump up to : `` The Kazakh Miracle : Recovery of the North Aral Sea ''. Environment News Service. 2008 - 08 - 01. Archived from the original on April 12, 2010. Retrieved 2010 - 03 - 22. 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Jump up ^ `` Soviet cotton threatens a region 's sea - and its children ''. New Scientist. November 18, 1989. Retrieved January 27, 2010. Jump up ^ USDA - Foreign Agriculture Service ( 2013 ). `` Cotton Production Ranking ''. National Cotton Council of America. Retrieved Oct 14, 2013. Jump up ^ `` ca-water.net, a knowledge base for projects in the Central Asia ''. 2003. Retrieved 1 November 2010. ^ Jump up to : Michael Wines ( 2002 - 12 - 09 ). `` Grand Soviet Scheme for Sharing Water in Central Asia Is Foundering ''. The New York Times. Retrieved 2008 - 03 - 08. Jump up ^ Bissell, Tom ( 2002 ). Eternal Winter : Lessons of the Aral Sea Disaster. Harper 's. pp. 41 -- 56. Jump up ^ Glantz, Michael H. ( 1999 ). Creeping Environmental Problems and Sustainable Development in the Aral Sea... Cambridge, New York : Cambridge University Press. p. 174. ISBN 0 - 521 - 62086 - 4. Retrieved May 17, 2008. Jump up ^ Craig Murray ( 2007 ). Dirty Diplomacy. Scribner. Jump up ^ Philip P. Micklin ( 1988 ). `` Desiccation of the Aral Sea ''. CIESIN, Columbia University. Retrieved January 6, 2013. ^ Jump up to : `` The Aral Sea Crisis ''. Thompson, Columbia University. Retrieved January 6, 2013. Jump up ^ `` Aral Sea - Aral Sea ''. Archived from the original on 2009 - 03 - 16. Jump up ^ Godwin O.P. Obasi ( February 11, 2003 ). `` Challenges and Opportunities in Water Resource Management '' ( PDF ). Lecture at the 93rd Annual Meeting of the American Meteorological Society. World Meteorological Organization. Jump up ^ `` Aral Sea ''. Encyclopædia Britannica. Encyclopædia Britannica Online. 2007. Retrieved May 17, 2008. Jump up ^ Dust Storm, Aral Sea Archived October 5, 2013, at the Wayback Machine., NASA Earth Observatory image, June 30, 2001 Jump up ^ Whish - Wilson, Phillip ( 2002 ). `` The Aral Sea environmental health crisis '' ( PDF ). Journal of Rural and Remote Environmental Health. 1 ( 2 ) : 30. Archived ( PDF ) from the original on April 9, 2008. Retrieved May 17, 2008. Jump up ^ Bland, Stephen M. ( 2015 - 01 - 27 ). `` Kazakhstan : Measuring the Northern Aral 's Comeback ''. EurasiaNet. Retrieved 2017 - 09 - 19. Jump up ^ `` Uzbekistan : Moynaq village faces the Aral Sea disaster ''. UNICEF. Jump up ^ Usmanova, RM ( 2013 - 03 - 25 ). `` Aral Sea and sustainable development ''. Water Sci Technol. 47 ( 7 - 8 ) : 41 -- 7. PMID 12793660. Jump up ^ Olli Varis. `` Resources : Curb vast water use in central Asia. ( Nature Vol 514 ( 7520 ) ) ''. Jump up ^ Ed Ring ( 2004 - 09 - 27 ). `` Release the Rivers : Let the Volga & Ob Refill the Aral Sea ''. Ecoworld. Archived from the original on April 29, 2008. Retrieved May 17, 2008. Jump up ^ `` Aral Sea Refill : Seawater Importation Macroproject ''. The Internet Encyclopedia of Science. June 29, 2008. Retrieved 2009 - 10 - 08. Jump up ^ `` Water - related vision for the Aral Sea Basin for the year 2025 ; 2000 '' ( PDF ). Retrieved 2013 - 06 - 12. Jump up ^ `` ( Nederland ) - UNESCO promotes unsustainable development in Central Asia ''. Indymedia NL. Retrieved July 18, 2009. Jump up ^ `` A Witch 's Brew ''. BBC News. July 2006. Archived from the original on December 13, 2007. Retrieved May 17, 2008. Jump up ^ Shawki Barghouti ( 2006 ). Case Study of the Aral Sea Water and Environmental Management Project : an independent evaluation of the World Bank 's support of regional programs. The World Bank ( Report ). Retrieved 1 November 2010. ^ Jump up to : Ilan Greenberg ( 2006 - 04 - 07 ). `` A vanished Sea Reclaims its form in Central Asia ''. Int. Her. Trib. Archived from the original on 12 May 2008. Retrieved May 17, 2008. Jump up ^ Ilan Greenberg ( 2006 - 04 - 06 ). `` As a Sea Rises, So Do Hopes for Fish, Jobs and Riches ''. The New York Times. Archived from the original on January 5, 2015. Retrieved 2008 - 05 - 16. Jump up ^ `` Miraculous Catch in Kazakhstan 's Northern Aral Sea ''. The World Bank. June 2006. Retrieved May 17, 2008. Jump up ^ `` North Aral Sea Recovery ''. The Earth Observatory. NASA. 2007. Retrieved 2008 - 05 - 17. ^ Jump up to : Martin Fletcher ( June 23, 2007 ). `` The return of the sea ''. The Times. London. Retrieved May 17, 2008. Jump up ^ `` Saving a Corner of the Aral Sea ''. The World Bank. 2005 - 09 - 01. Retrieved May 17, 2008. Jump up ^ `` The rehabilitation of the ecosystem and bioproductivity of the Aral Sea under conditions of water scarcity '' ( PDF ). August 2007. Jump up ^ `` Strategies suggested for implementation ''. ICWC. Retrieved January 6, 2013. Jump up ^ `` IFAS ''. WaterWiki.net. Retrieved April 4, 2010. Jump up ^ NASA Visible Earth - `` Rebirth '' Island Joins the Mainland Archived 2010 - 05 - 28 at the Wayback Machine., Aral Sea Archived 2010 - 07 - 28 at the Wayback Machine. Jump up ^ Bozheyeva, G., Y. Kunakbayev and D. Yeleukenov ( 1999 ). Former Soviet Biological Weapons Facilities in Kazakhstan : Past, Present and Future. Occasional Paper 1. Monterey, Calif. : Monterey Institute of International Studies, Center for Nonproliferation Studies. CS1 maint : Uses authors parameter ( link ) Jump up ^ Khabar Television / BBC Monitoring ( November 20, 2002 ). `` Kazakhstan : Vozrozhdeniya Anthrax Burial Sites Destroyed ''. Global Security Newswire. Nuclear Threat Initiative. Archived from the original on April 22, 2008. Retrieved May 17, 2008. CS1 maint : Uses authors parameter ( link ) Jump up ^ `` Uzbekistan, intl consortium ink deal on exploring Aral Sea ''. ITAR - Tass. Archived from the original on 2010 - 07 - 27. Jump up ^ Michael Hancock - Parmer ( 2010 - 06 - 09 ). `` Aral Gas ''. Registan.net. Archived from the original on 2010 - 06 - 11. Jump up ^ `` Psy ''. Kino Expert. Retrieved September 18, 2009. Jump up ^ `` Delta Blues ( in a land of cotton ) ''. YouTube. November 5, 2008. Retrieved July 18, 2009. Jump up ^ Al Jazeera World. `` People of the Lake ''. Retrieved 4 December 2015. Jump up ^ `` Watch Pink Floyd 's Surreal, Sun - Baked ' Louder Than Words ' Video ''. Rolling Stone. Retrieved 4 December 2015. Further reading Micklin, Philip ( 2007 ). `` The Aral Sea Disaster ''. Annual Review of Earth and Planetary Sciences. 35 ( 4 ) : 47 -- 72. doi : 10.1146 / annurev. earth. 35.031306. 140120. Retrieved May 17, 2008. Bissell, Tom ( April 2002 ). `` Eternal Winter : Lessons of the Aral Sea Disaster ''. Harper 's. pp. 41 -- 56. Retrieved May 17, 2008. Bissell, Tom ( 2004 ). Chasing The Sea : Lost Among the Ghosts of Empire in Central Asia. New York : Vintage Books. ISBN 978 - 0 - 375 - 72754 - 2. Ellis, William S ( February 1990 ). `` A Soviet Sea Lies Dying ''. National Geographic. pp. 73 -- 93. Ferguson, Rob ( 2003 ). The Devil and the Disappearing Sea. Vancouver : Raincoast Books. ISBN 1 - 55192 - 599 - 0. Kasperson, Jeanne ; Kasperson, Roger ; Turner, B.L ( 1995 ). The Aral Sea Basin : A Man - Made Environmental Catastrophe. Dordrecht ; Boston : Kluwer Academic Publishers. p. 92. ISBN 92 - 808 - 0848 - 6. Bendhun, François ; Renard, Philippe ( 2004 ). `` Indirect estimation of groundwater inflows into the Aral sea via a coupled water and salt mass balance model ''. Journal of Marine Systems. 47 ( 1 - 4 ) : 35 -- 50. doi : 10.1016 / j. jmarsys. 2003.12. 007. Archived from the original on February 14, 2008. Retrieved May 17, 2008. Sirjacobs, Damien ; Grégoire, Marilaure ; Delhez, Eric ; Nihoul, JCJ ( 2004 ). `` Influence of the Aral Sea negative water balance on its seasonal circulation patterns : use of a 3D hydrodynamic model ''. Journal of Marine Systems. 47 ( 1 - 4 ) : 51 -- 66. doi : 10.1016 / j. jmarsys. 2003.12. 008. External links Wikivoyage has a travel guide for Aral Sea. Wikimedia Commons has media related to Aral Sea. Rivers Network : Aral Sea watersheds - webmap Post-Soviet Legacy : Aral Sea Pollution from the Dean Peter Krogh Foreign Affairs Digital Archives Aral Sea Foundation Union for Defence of the Aral Sea and Amudarya River `` Syr Darya Control & Northern Aral Sea Phase I Project ''. World Bank Group - Kazakhstan. December 2006. Aral Sea from Space ( time lapse ) Swedish Aral Sea Society Google Earth view of the Aral Sea Regions of the world Regions of Africa Central Africa Guinea region Gulf of Guinea Cape Lopez Mayombe Igboland Mbaise Maputaland Pool Malebo Congo Basin Chad Basin Congolese rainforests Ouaddaï highlands Ennedi Plateau East Africa African Great Lakes Albertine Rift East African Rift Great Rift Valley Gregory Rift Rift Valley lakes Swahili coast Virunga Mountains Kavirondo Zanj Serengeti Horn of Africa Afar Triangle Al - Habash Barbara Danakil Alps Danakil Desert Ethiopian Highlands Gulf of Aden Gulf of Tadjoura Indian Ocean islands Comoros Islands North Africa Maghreb Ifriqiya Barbary Coast Bashmur Ancient Libya Atlas Mountains Nile Valley Cataracts of the Nile Darfur Gulf of Aqaba Lower Egypt Lower Nubia Middle Egypt Nile Delta Nuba Mountains Nubia The Sudans Upper Egypt Western Sahara West Africa Pepper Coast Gold Coast Slave Coast Ivory Coast Cape Palmas Cape Mesurado Guinea region Gulf of Guinea Niger Basin Guinean Forests of West Africa Niger Delta Inner Niger Delta Southern Africa Madagascar Central Highlands ( Madagascar ) Northern Highlands Rhodesia North South Thembuland Succulent Karoo Nama Karoo Bushveld Highveld Fynbos Cape Floristic Region Kalahari Desert Okavango Delta Cape Peninsula False Bay Hydra Bay Macro-regions Aethiopia Arab world Commonwealth realm East African montane forests Eastern Desert Equatorial Africa Françafrique Gibraltar Arc Greater Middle East Islands of Africa List of countries where Arabic is an official language Mediterranean Basin MENA MENASA Middle East Mittelafrika Negroland Northeast Africa Portuguese - speaking African countries Sahara Sahel Sub-Saharan Africa Sudan ( region ) Sudanian Savanna Tibesti Mountains Tropical Africa Regions of Asia Central Greater Middle East Aral Sea Aralkum Desert Caspian Sea Dead Sea Sea of Galilee Transoxiana Turan Greater Khorasan Ariana Khwarezm Sistan Kazakhstania Eurasian Steppe Asian Steppe Kazakh Steppe Pontic -- Caspian steppe Mongolian - Manchurian grassland Wild Fields Yedisan Muravsky Trail Ural Ural Mountains Volga region Idel - Ural Kolyma Transbaikal Pryazovia Bjarmaland Kuban Zalesye Ingria Novorossiya Gornaya Shoriya Tulgas Iranian Plateau Altai Mountains Pamir Mountains Tian Shan Badakhshan Wakhan Corridor Wakhjir Pass Mount Imeon Mongolian Plateau Western Regions Taklamakan Desert Karakoram Trans - Karakoram Tract Siachen Glacier North Inner Asia Northeast Far East Russian Far East Okhotsk - Manchurian taiga Extreme North Siberia Baikalia ( Lake Baikal ) Transbaikal Khatanga Gulf Baraba steppe Kamchatka Peninsula Amur Basin Yenisei Gulf Yenisei Basin Beringia Sikhote - Alin East Orient Japanese archipelago Northeastern Japan Arc Sakhalin Island Arc Korean Peninsula Gobi Desert Taklamakan Desert Greater Khingan Mongolian Plateau Inner Asia Inner Mongolia Outer Mongolia China proper Manchuria Outer Manchuria Inner Manchuria Northeast China Plain Mongolian - Manchurian grassland North China Plain Yan Mountains Kunlun Mountains Liaodong Peninsula Himalayas Tibetan Plateau Tibet Tarim Basin Northern Silk Road Hexi Corridor Nanzhong Lingnan Liangguang Jiangnan Jianghuai Guanzhong Huizhou Wu Jiaozhou Zhongyuan Shaannan Ordos Loop Loess Plateau Shaanbei Hamgyong Mountains Central Mountain Range Japanese Alps Suzuka Mountains Leizhou Peninsula Gulf of Tonkin Yangtze River Delta Pearl River Delta Yenisei Basin Altai Mountains Wakhan Corridor Wakhjir Pass West Greater Middle East MENA MENASA Middle East Red Sea Caspian Sea Mediterranean Sea Zagros Mountains Persian Gulf Pirate Coast Strait of Hormuz Greater and Lesser Tunbs Al - Faw Peninsula Gulf of Oman Gulf of Aqaba Gulf of Aden Balochistan Arabian Peninsula Najd Hejaz Tihamah Eastern Arabia South Arabia Hadhramaut Arabian Peninsula coastal fog desert Tigris -- Euphrates Mesopotamia Upper Mesopotamia Lower Mesopotamia Sawad Nineveh plains Akkad ( region ) Babylonia Canaan Aram Aram - Naharaim Eber - Nari Suhum Eastern Mediterranean Mashriq Kurdistan Levant Southern Levant Transjordan Jordan Rift Valley Israel Levantine Sea Golan Heights Hula Valley Galilee Gilead Judea Samaria Arabah Anti-Lebanon Mountains Sinai Peninsula Arabian Desert Syrian Desert Fertile Crescent Azerbaijan Syria Palestine Iranian Plateau Armenian Highlands Caucasus Caucasus Mountains Greater Caucasus Lesser Caucasus North Caucasus South Caucasus Kur - Araz Lowland Lankaran Lowland Alborz Absheron Peninsula Anatolia Cilicia Cappadocia Alpide belt South Orient Greater India Indian subcontinent Himalayas Hindu Kush Carnatic region Western Ghats Eastern Ghats Ganges Basin Ganges Delta Pashtunistan Punjab Balochistan Kashmir Kashmir Valley Pir Panjal Range Thar Desert Indus Valley Indus River Delta Indus Valley Desert Indo - Gangetic Plain Eastern coastal plains Western Coastal Plains Meghalaya subtropical forests MENASA Lower Gangetic plains moist deciduous forests Northwestern Himalayan alpine shrub and meadows Doab Bagar tract Great Rann of Kutch Little Rann of Kutch Deccan Plateau Coromandel Coast Konkan False Divi Point Hindi Belt Ladakh Aksai Chin Gilgit - Baltistan Baltistan Shigar Valley Karakoram Saltoro Mountains Siachen Glacier Bay of Bengal Gulf of Khambhat Gulf of Kutch Gulf of Mannar Trans - Karakoram Tract Wakhan Corridor Wakhjir Pass Lakshadweep Andaman and Nicobar Islands Andaman Islands Nicobar Islands Maldive Islands Alpide belt Southeast Orient Sundaland Mainland Indochina Malay Peninsula Maritime Peninsular Malaysia Sunda Islands Greater Sunda Islands Lesser Sunda Islands Indonesian Archipelago Wallacea Timor New Guinea Bonis Peninsula Papuan Peninsula Huon Peninsula Huon Gulf Bird 's Head Peninsula Gazelle Peninsula Philippine Archipelago Luzon Visayas Mindanao Leyte Gulf Gulf of Thailand East Indies Nanyang Alpide belt Asia - Pacific Tropical Asia Ring of Fire Regions of Europe North Nordic Northwestern Scandinavia Scandinavian Peninsula Fennoscandia Baltoscandia Sápmi West Nordic Baltic Baltic Sea Gulf of Bothnia Gulf of Finland Iceland Faroe Islands East Danubian countries Prussia Galicia Volhynia Donbass Sloboda Ukraine Sambia Peninsula Amber Coast Curonian Spit Izyum Trail Lithuania Minor Nemunas Delta Baltic Baltic Sea Vyborg Bay Karelia East Karelia Karelian Isthmus Lokhaniemi Southeastern Balkans Aegean Islands Gulf of Chania North Caucasus Greater Caucasus Kabardia European Russia Southern Russia Central Baltic Baltic Sea Alpine states Alpide belt Mitteleuropa Visegrád Group West Benelux Low Countries Northwest British Isles English Channel Channel Islands Cotentin Peninsula Normandy Brittany Gulf of Lion Iberia Al - Andalus Baetic System Pyrenees Alpide belt South Italian Peninsula Insular Italy Tuscan Archipelago Aegadian Islands Iberia Al - Andalus Baetic System Gibraltar Arc Southeastern Mediterranean Crimea Alpide belt Germanic Romance Celtic Slavic countries Uralic European Plain Eurasian Steppe Pontic -- Caspian steppe Wild Fields Pannonian Basin Great Hungarian Plain Little Hungarian Plain Eastern Slovak Lowland Regions of North America Northern Eastern Canada Western Canada Canadian Prairies Central Canada Northern Canada Atlantic Canada The Maritimes French Canada English Canada Acadia Acadian Peninsula Quebec City -- Windsor Corridor Peace River Country Cypress Hills Palliser 's Triangle Canadian Shield Interior Alaska - Yukon lowland taiga Newfoundland ( island ) Vancouver Island Gulf Islands Strait of Georgia Canadian Arctic Archipelago Labrador Peninsula Gaspé Peninsula Avalon Peninsula Bay de Verde Peninsula Brodeur Peninsula Melville Peninsula Bruce Peninsula Banks Peninsula ( Nunavut ) Cook Peninsula Gulf of Boothia Georgian Bay Hudson Bay James Bay Greenland Pacific Northwest Inland Northwest Northeast New England Mid-Atlantic Commonwealth West Midwest Upper Midwest Mountain states Intermountain West Basin and Range Province Oregon Trail Mormon Corridor Calumet Region Southwest Old Southwest Llano Estacado Central United States Tallgrass prairie South South Central Deep South Upland South Four Corners East Coast West Coast Gulf Coast Third Coast Eastern United States Appalachia Trans - Mississippi Great North Woods Great Plains Interior Plains Great Lakes Great Basin Great Basin Desert Acadia Ozarks Ark - La - Tex Waxhaws Siouxland Twin Tiers Driftless Area Palouse Piedmont Atlantic coastal plain Outer Lands Black Dirt Region Blackstone Valley Piney Woods Rocky Mountains Mojave Desert The Dakotas The Carolinas Shawnee Hills San Fernando Valley Tornado Alley North Coast Lost Coast Emerald Triangle San Francisco Bay Area San Francisco Bay North Bay East Bay Silicon Valley Interior Alaska - Yukon lowland taiga Gulf of Mexico Lower Colorado River Valley Sacramento -- San Joaquin River Delta Yukon -- Kuskokwim Delta Colville Delta Arkansas Delta Mobile -- Tensaw River Delta Mississippi Delta Mississippi River Delta Columbia River Estuary Great Basin High Desert Monterey Peninsula Upper Peninsula of Michigan Lower Peninsula of Michigan Virginia Peninsula Keweenaw Peninsula Middle Peninsula Delmarva Peninsula Alaska Peninsula Kenai Peninsula Niagara Peninsula Beringia Belt regions Bible Belt Black Belt Corn Belt Cotton Belt Frost Belt Rice Belt Rust Belt Sun Belt Snow Belt Latin Northern Mexico Baja California Peninsula Gulf of California Colorado River Delta Gulf of Mexico Soconusco Tierra Caliente La Mixteca La Huasteca Bajío Valley of Mexico Mezquital Valley Sierra Madre de Oaxaca Yucatán Peninsula Basin and Range Province Western Caribbean Zone Isthmus of Panama Gulf of Panama Pearl Islands Azuero Peninsula Mosquito Coast West Indies Antilles Greater Antilles Lesser Antilles Leeward Leeward Antilles Windward Lucayan Archipelago Southern Caribbean Aridoamerica Mesoamerica Oasisamerica Northern Middle Anglo Latin French Hispanic American Cordillera Ring of Fire LAC Regions of Oceania Australasia Gulf of Carpentaria Zealandia Kula Gulf Australia Capital Country Eastern Australia Lake Eyre basin Murray -- Darling basin Northern Australia Nullarbor Plain Outback Southern Australia Maralinga Sunraysia Great Victoria Desert Gulf of Carpentaria Gulf St Vincent Lefevre Peninsula Fleurieu Peninsula Yorke Peninsula Eyre Peninsula Mornington Peninsula Bellarine Peninsula Mount Henry Peninsula Melanesia Islands Region Bismarck Archipelago Solomon Islands North Solomon Islands Solomon Islands Fiji New Caledonia New Guinea Papua New Guinea Republic of West Papua Vanuatu Micronesia Caroline Islands Federated States of Micronesia Palau Kiribati Mariana Islands Guam Northern Mariana Islands Marshall Islands Nauru Wake Island Polynesia Easter Island Hawaiian Islands Cook Islands French Polynesia Austral Islands Gambier Islands Mangareva Islands Marquesas Islands Society Islands Tuamotu Kermadec Islands New Zealand South Island North Island Niue Pitcairn Islands Samoan Islands American Samoa Independent State of Samoa Tokelau Tonga Tuvalu Ring of Fire Regions of South America East Amazon basin Atlantic Forest Caatinga Cerrado North Caribbean South America West Indies Los Llanos The Guianas Amazon basin Amazon rainforest Gulf of Paria Paria Peninsula Paraguaná Peninsula Orinoco Delta South Tierra del Fuego Patagonia Pampas Pantanal Gran Chaco Chiquitano dry forests Valdes Peninsula West Andes Tropical Andes Wet Andes Dry Andes Pariacaca mountain range Altiplano Atacama Desert Latin Hispanic American Cordillera Ring of Fire LAC Polar regions Antarctic Antarctic Peninsula East Antarctica West Antarctica Eklund Islands Ecozone Extreme points Islands Arctic Arctic Alaska British Arctic Territories Canadian Arctic Archipelago Finnmark Greenland Northern Canada Northwest Territories Nunavik Nunavut Russian Arctic Sakha Sápmi Yukon North American Arctic Earth 's oceans and seas Arctic Ocean Amundsen Gulf Barents Sea Beaufort Sea Chukchi Sea East Siberian Sea Greenland Sea Gulf of Boothia Kara Sea Laptev Sea Lincoln Sea Prince Gustav Adolf Sea Pechora Sea Queen Victoria Sea Wandel Sea White Sea Atlantic Ocean Adriatic Sea Aegean Sea Alboran Sea Archipelago Sea Argentine Sea Baffin Bay Balearic Sea Baltic Sea Bay of Biscay Bay of Bothnia Bay of Campeche Bay of Fundy Black Sea Bothnian Sea Caribbean Sea Celtic Sea English Channel Foxe Basin Greenland Sea Gulf of Bothnia Gulf of Finland Gulf of Lion Gulf of Guinea Gulf of Maine Gulf of Mexico Gulf of Saint Lawrence Gulf of Sidra Gulf of Venezuela Hudson Bay Ionian Sea Irish Sea Irminger Sea James Bay Labrador Sea Levantine Sea Libyan Sea Ligurian Sea Marmara Sea Mediterranean Sea Myrtoan Sea North Sea Norwegian Sea Sargasso Sea Sea of Åland Sea of Azov Sea of Crete Sea of the Hebrides Thracian Sea Tyrrhenian Sea Wadden Sea Indian Ocean Andaman Sea Arabian Sea Bali Sea Bay of Bengal Flores Sea Great Australian Bight Gulf of Aden Gulf of Aqaba Gulf of Khambhat Gulf of Kutch Gulf of Oman Gulf of Suez Java Sea Laccadive Sea Mozambique Channel Persian Gulf Red Sea Timor Sea Pacific Ocean Arafura Sea Banda Sea Bering Sea Bismarck Sea Bohai Sea Bohol Sea Camotes Sea Celebes Sea Ceram Sea Chilean Sea Coral Sea East China Sea Gulf of Alaska Gulf of Anadyr Gulf of California Gulf of Carpentaria Gulf of Fonseca Gulf of Panama Gulf of Thailand Gulf of Tonkin Halmahera Sea Koro Sea Mar de Grau Molucca Sea Moro Gulf Philippine Sea Salish Sea Savu Sea Sea of Japan Sea of Okhotsk Seto Inland Sea Shantar Sea Sibuyan Sea Solomon Sea South China Sea Sulu Sea Tasman Sea Visayan Sea Yellow Sea Southern Ocean Amundsen Sea Bellingshausen Sea Cooperation Sea Cosmonauts Sea Davis Sea D'Urville Sea King Haakon VII Sea Lazarev Sea Mawson Sea Riiser - Larsen Sea Ross Sea Scotia Sea Somov Sea Weddell Sea Landlocked seas Aral Sea Caspian Sea Dead Sea Salton Sea Book Category Earth 's oceans and seas Arctic Ocean Amundsen Gulf Barents Sea Beaufort Sea Chukchi Sea East Siberian Sea Greenland Sea Gulf of Boothia Kara Sea Laptev Sea Lincoln Sea Prince Gustav Adolf Sea Pechora Sea Queen Victoria Sea Wandel Sea White Sea Atlantic Ocean Adriatic Sea Aegean Sea Alboran Sea Archipelago Sea Argentine Sea Baffin Bay Balearic Sea Baltic Sea Bay of Biscay Bay of Bothnia Bay of Campeche Bay of Fundy Black Sea Bothnian Sea Caribbean Sea Celtic Sea English Channel Foxe Basin Greenland Sea Gulf of Bothnia Gulf of Finland Gulf of Lion Gulf of Guinea Gulf of Maine Gulf of Mexico Gulf of Saint Lawrence Gulf of Sidra Gulf of Venezuela Hudson Bay Ionian Sea Irish Sea Irminger Sea James Bay Labrador Sea Levantine Sea Libyan Sea Ligurian Sea Marmara Sea Mediterranean Sea Myrtoan Sea North Sea Norwegian Sea Sargasso Sea Sea of Åland Sea of Azov Sea of Crete Sea of the Hebrides Thracian Sea Tyrrhenian Sea Wadden Sea Indian Ocean Andaman Sea Arabian Sea Bali Sea Bay of Bengal Flores Sea Great Australian Bight Gulf of Aden Gulf of Aqaba Gulf of Khambhat Gulf of Kutch Gulf of Oman Gulf of Suez Java Sea Laccadive Sea Mozambique Channel Persian Gulf Red Sea Timor Sea Pacific Ocean Arafura Sea Banda Sea Bering Sea Bismarck Sea Bohai Sea Bohol Sea Camotes Sea Celebes Sea Ceram Sea Chilean Sea Coral Sea East China Sea Gulf of Alaska Gulf of Anadyr Gulf of California Gulf of Carpentaria Gulf of Fonseca Gulf of Panama Gulf of Thailand Gulf of Tonkin Halmahera Sea Koro Sea Mar de Grau Molucca Sea Moro Gulf Philippine Sea Salish Sea Savu Sea Sea of Japan Sea of Okhotsk Seto Inland Sea Shantar Sea Sibuyan Sea Solomon Sea South China Sea Sulu Sea Tasman Sea Visayan Sea Yellow Sea Southern Ocean Amundsen Sea Bellingshausen Sea Cooperation Sea Cosmonauts Sea Davis Sea D'Urville Sea King Haakon VII Sea Lazarev Sea Mawson Sea Riiser - Larsen Sea Ross Sea Scotia Sea Somov Sea Weddell Sea Landlocked seas Aral Sea Caspian Sea Dead Sea Salton Sea Book Category Lakes of Kazakhstan Caspian Sea Aike Alakol Aral North South Balkhash Barak Kol Bartogay Chagan Issyk Jasybay Kayindi Kopa Kamyslybas Markakol Sasykkol Siletiteniz Tengiz Zaysan Zerendi Zhasylkol NDL : 00651085 Retrieved from `` https://en.wikipedia.org/w/index.php?title=Aral_Sea&oldid=849615682 '' Categories : Aral Sea Endorheic lakes of Asia Environmental disasters in Asia Geography of Central Asia Shrunken lakes Former lakes Lakes of Kazakhstan Lakes of Uzbekistan Saline lakes Kazakhstan -- Uzbekistan border International lakes of Asia Hidden categories : Webarchive template wayback links CS1 maint : Uses authors parameter Articles containing Kazakh - language text Articles containing Uzbek - language text Articles containing Russian - language text Coordinates on Wikidata All articles with unsourced statements Articles with unsourced statements from July 2014 Articles containing potentially dated statements from 2008 All articles containing potentially dated statements Wikipedia articles needing clarification from July 2014 Articles with unsourced statements from November 2017 All articles with vague or ambiguous time Vague or ambiguous time from July 2014 Wikipedia articles needing clarification 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Question: the eastern half of this one large central asian sea is now completely dry
Answer: Aral Sea