"World Discoveries III: Dead Sea World Discoveries III: Dead Sea is a 1999 documentary that takes an in-depth look at the Dead Sea, which is a lake on the border between Israel and Jordan. At 8.6 times saltier than the ocean, the Dead Sea is so salty fish can't swim in it, boats can't sail on it, and animals can't survive around it. The film explores the ominous reputation the salty body of water has acquired and shows slow wide-screen nature shots of its surroundings. ""World Discoveries III - Dead Sea"" travels around the Dead Sea to explore its history"
"Salton Sea The Salton Sea is a shallow, saline, endorheic rift lake located directly on the San Andreas Fault, predominantly in the U.S. state of California's Imperial and Coachella valleys. The lake occupies the lowest elevations of the Salton Sink in the Colorado Desert of Imperial and Riverside counties in Southern California. Its surface is below sea level as of January 2018. The deepest point of the sea is higher than the lowest point of Death Valley. The sea is fed by the New, Whitewater, and Alamo Rivers, as well as agricultural runoff, drainage systems, and creeks. Over millions of"
"The proposal was withdrawn after several lawsuits, and is regarded as an important exercise of native rights in the United States. Zuni Salt Lake Zuni Salt Lake, also Zuñi Salt Lake is a rare high desert lake, and a classic maar. It is located in Catron County, about 60 miles south of the Zuni Pueblo, New Mexico, USA. Zuñi Salt Lake is extremely shallow, with a depth of only four feet in the wet season. During the dry season, much of the water evaporates leaving behind saltflats. It was listed on the National Register of Historic Places in 1999. It"
"Lake Vanda Lake Vanda is a lake in Wright Valley, Victoria Land, Ross Dependency, Antarctica. The lake is 5 km long and has a maximum depth of 69 m. On its shore, New Zealand maintained Vanda Station from 1968 to 1995. Lake Vanda is a hypersaline lake with a salinity more than ten times that of seawater, more than the salinity of the Dead Sea, and perhaps even more than of Lake Assal (Djibouti), which is the world's most saline lake outside of Antarctica. Lake Vanda is also meromictic, which means that the deeper waters of the lake don't mix"
"Namak Lake Namak Lake (, i.e., ""salt lake"") is a salt lake in Iran. It is located approximately east of the City of Qom and of Kashan at an elevation of above sea level. The lake is a remnant of the Paratethys sea, which started to dry from the Pleistocene epoch, leaving Lake Urmia and the Caspian Sea and other bodies of water. The lake has a surface area of about , but most of this is dry. Water only covers . The lake only reaches a depth between to . The most important water supply is the river Qom."
"Namak Lake Namak Lake (, i.e., ""salt lake"") is a salt lake in Iran. It is located approximately east of the City of Qom and of Kashan at an elevation of above sea level. The lake is a remnant of the Paratethys sea, which started to dry from the Pleistocene epoch, leaving Lake Urmia and the Caspian Sea and other bodies of water. The lake has a surface area of about , but most of this is dry. Water only covers . The lake only reaches a depth between to . The most important water supply is the river Qom."
"Zuni Salt Lake Zuni Salt Lake, also Zuñi Salt Lake is a rare high desert lake, and a classic maar. It is located in Catron County, about 60 miles south of the Zuni Pueblo, New Mexico, USA. Zuñi Salt Lake is extremely shallow, with a depth of only four feet in the wet season. During the dry season, much of the water evaporates leaving behind saltflats. It was listed on the National Register of Historic Places in 1999. It is part of the Red Hill volcanic field. For centuries, the Pueblo people of the Southwest, including the Zuni, Acoma, Laguna,"
"Lake Baskunchak Lake Baskunchak () is a salt lake of 115 km² in Astrakhan Oblast, Russia, located at , about 270 km north of the Caspian Sea, and 53 km east of the Volga. Since 1997 the area is protected as part of the Bogdinsko-Baskunchakski Nature Reserve. The surface elevation of the lake is 21 m below sea level. It is fed by a river that draws from an area of 11,000 km². The salinity of the lake is about 300 g/l. Since the 8th century its salt was mined and traded along the Silk Road. Nowadays the lake's salt"
"Lake Baskunchak Lake Baskunchak () is a salt lake of 115 km² in Astrakhan Oblast, Russia, located at , about 270 km north of the Caspian Sea, and 53 km east of the Volga. Since 1997 the area is protected as part of the Bogdinsko-Baskunchakski Nature Reserve. The surface elevation of the lake is 21 m below sea level. It is fed by a river that draws from an area of 11,000 km². The salinity of the lake is about 300 g/l. Since the 8th century its salt was mined and traded along the Silk Road. Nowadays the lake's salt"
"Mahoney Lake Mahoney Lake is a meromictic saline lake located near Okanagan Falls in British Columbia, Canada. It was established as an ecological reserve to preserve a southern interior saline lake, possessing unique limnological features in 1972. It has a unique layering, where the very bottom of the lake is very salt rich and contains hydrogen sulphide (HS), which facilitates the growth of the purple sulphur bacteria in the layer above it, where the bacteria has just enough light to grow. The upper layer of the lake consists of a mixing layer of fresh water. Mahoney Lake is alkaline because"
"Limassol Salt Lake Limassol Salt Lake (also known as Akrotiri Salt Lake) is the largest inland body of water on the island of Cyprus, in Akrotiri and Dhekelia, United Kingdom, an overseas territory. It lies due south-west of the sprawling city of Limassol and measures 10.65 km. Its lowest point is 2.7 meters below sea level and at its deepest point the water depth measures about one meter. Geologists hypothesize the lake was formed over the gradual joining of an offshore islet off the southern coast of Cyprus. The lake itself is considered to be one of the eastern Mediterranean"
"Tathlina Lake Tathlina Lake is a large, shallow lake, located in the Northwest Territories, Canada. An outcropping of the Kakisa Formation occurs along the side of this lake. This turbid lake, the 15th largest in the Northwest Territories, is located at an elevation of 269 metres, and has an average depth of only 1 metre. Due to this shallow depth, it is considered vulnerable to changes in such variables as water level and temperature, ice thickness, and dissolved oxygen levels. It has also been subject to fish kills. Commercial fishing for walleye ""(Sander vitreus)"" commenced in 1953. However, during the"
"is 4 times more saline than the ocean, hot water up to , and cold water down to . This species is known from only two locations in Death Valley: Salt Creek (subspecies ""salinus"") at about 49 meters below sea level, and Cottonball Marsh (subspecies ""milleri""), at about 80 meters below sea level. They are thought to be the remainders of a large ecosystem of fish species that lived in Lake Manly, which dried up at the end of the last ice age leaving the present day Death Valley. The Salt Creek subspecies is also found at River Springs and"
"it features no inflow or outflow of water. The lake also contains very low levels of oxygen and an approximate pH of 7.5-9.0. The surface area of the lake is 18ha and the surface area of the land is 21ha, with combined total of 21 ha. Mahoney Lake Mahoney Lake is a meromictic saline lake located near Okanagan Falls in British Columbia, Canada. It was established as an ecological reserve to preserve a southern interior saline lake, possessing unique limnological features in 1972. It has a unique layering, where the very bottom of the lake is very salt rich and"
"Organic Lake Organic Lake is a lake in the Vestfold Hills in eastern Antarctica. It was formed 6,000 years ago when sea levels were higher; it is isolated, rather shallow (7.5m), meromictic, a few hundred meters in diameter and has extremely salty water. It has the highest recorded concentration of dimethyl sulfide in any natural body of water. In 2011, a new species of virophage (a satellite virus that impairs the ability of its co-infective host virus to replicate) was discovered in Organic Lake, the Organic Lake virophage. It is a parasite of 'Organic Lake phycodnavirus', a large virus that"
"occur. However, other factors such as hydrothermal vents, diffusion of salt from minerals and sediment, including concentrated brine, and evaporites are another contributor to salinity, as is the recent lowering of lake levels raising the salinity, though sedimentary records show the lake surface elevation reached levels 10–12 m above world sea level in the 1500s. The temperature of the surface water changes with the seasonally varying air temperature. Winter lows can reach temperatures as low as and summer highs can reach . http://water.ca.gov/LegacyFiles/pubs/conservation/salton_sea_history/history.pdf Salton Sea The Salton Sea is a shallow, saline, endorheic rift lake located directly on the San"
"of sand dunes. Its elevation is 325 metres (1066ft) above mean sea level. In indigenous culture, ""Kumpupintil"" was off-limits to the tribes neighbouring the area, such as the Kurajarra, Wanman, Kartudjara and the Putidjara. The reason for the taboo, existing down to modern times, derives from the lake's mythological associations with the ""Ngayurnangalku"" spirits thought to live below its surface. This prohibition extended to flying over the area, since the Ngayurnangalku, ancestral cannibal beings with pointy teeth and clawlike fingernails, are deemed capable of ripping even planes that intrude over the lake's airspace. The lake is home to many species"
"Tuyajto Lake Tuyajto Lake is a salt lake located in the Antofagasta Region, northern Chile. Located at an elevation of about , its surface area presently fluctuates between but in the past it was considerably larger; this led to humans going to the lake and creating archeological sites there. Presently, the lake is groundwater-fed and has no surface outlet but water might seep out underground. The lake lies at an elevation of . It has a maximum depth of while its surface area varies seasonally from in summer to in winter when the lake is sometimes partially frozen over; at"
"in the continental interior of the United States and the third-lowest spot in the interior of the North American continent after Iliamna Lake in Alaska (942 feet [287 m] below sea level) and Great Slave Lake in the Northwest Territories of Canada at ( below sea level). (Though Crater Lake is the deepest lake in the United States and deeper than Lake Superior, Crater Lake's elevation is higher and consequently its deepest point is ""above"" sea level.) While the temperature of the surface of Lake Superior varies seasonally, the temperature below is an almost constant 39 °F (4 °C). This"
"lakes in the Kumkol basin of the reserve: Lake Ayakum, Lake Aqqikkal, and Lake Jingyu. All are saline (""salt lakes""). The northernmost, Lake Ayakum, is at an altitude of 12,685 feet and has an area of 283 sqmi. Its depth reaches 74 feet. To the west of Lake Ayakum is Lake Aqqikkal, at an altitude of 13,940 ft, and which is 16 miles across. Lake Jingyu is the southernmost. Because of its high altitude (over 4,500 meters above sea level) and arid location thousands of kilometers from any ocean and in the rain shadow of the Himalayas and other mountain,"
"Pacific Tarn Pacific Tarn is a small lake located in the Colorado Rocky Mountains in the United States. It is notable for its 13,420 foot (4,090 m) elevation, making it the highest lake in the United States whose name is recognized by the United States Board on Geographic Names. The lake sits atop the broad eastern ridge of Pacific Peak in the Tenmile Range. Efforts to name the lake were spearheaded by Carl Drews, a Boulder, Colorado resident who organized an expedition to the lake in 2002 to measure the size, depth and water chemistry. The lake remained unnamed until"
"Harney Lake Harney Lake is a shallow alkali lake basin located in southeast Oregon, United States, approximately south of the city of Burns. The lake lies within the boundary of the Malheur National Wildlife Refuge and is the lowest point in the Blitzen Valley drainage. The lake has been known by several names, including Salt Lake in 1838, Tonowama, and Lake Harney. Despite a history of 9,000 years of human inhabitation on Harney Lake by the Northern Paiute Indians primarily as nomadic wintering camps, little sign of modern human habitation is evident on Harney Lake. The nearest residents live in"
"L'Atalante basin L'Atalante basin is a hypersaline brine lake at the bottom of the Mediterranean Sea about west of the island of Crete. It is named for the French ""L'Atalante"", one of the oceanographic research vessels involved in its discovery in 1993. L'Atalante and its neighbors the Urania and Discovery deep hyper saline anoxic basins (DHABs) are at most 35,000 years old. They were formed by Messinian evaporite salt deposits dissolving out of the Mediterranean Ridge and collecting in abyssal depressions about deep. L'Atalante is the smallest of the three; its surface begins at about below sea level. The L'Atalante"
"Ayding Lake Aydingkol (), Aydingkul (Mongol) or Ayding () is a lake in the Turpan Depression, Xinjiang Uyghur Autonomous Region, PR China. At 154 m below sea level, it is the lowest point in China, and also lower than anywhere on Earth outside the countries of Israel, Jordan, Palestine, Syria, and Djibouti. This lake is now totally dried, and very muddy and salty. In ancient times, Ayding Lake was known as ""juéluòwǎn"" (觉洛浣). The Uyghur derived name ""Aydingköl"" means ""moon lake"", due to the lake having a layer of white salt along its edge, giving the appearance of a shining"
"level is the goal, a goal made more difficult during years of drought in the American West. Mono Lake Mono Lake ( ) is a large, shallow saline soda lake in Mono County, California, formed at least 760,000 years ago as a terminal lake in an endorheic basin. The lack of an outlet causes high levels of salts to accumulate in the lake. These salts also make the lake water alkaline. This desert lake has an unusually productive ecosystem based on brine shrimp that thrive in its waters, and provides critical habitat for two million annual migratory birds that feed"
"lake is located in the Gangdise Mountains (also known as the Lunggar Mountains) deep in the Tibetan Plateau. It is one of 251 salt lakes in Tibet. It is divided into the northern (98 km²) and the southern (149 km²) sub-basins, which are linked by a narrow channel. The southern part is semi-dry and appears white in satellite images. The northern part is fed from two inlets on east and on the west, by the snow melt of the Rianglinag Mountains (). The catchment area is 6,680 km², and the lake is surrounded by mountains with a height of 4,600–5,200"
"site. Spotted Lake Spotted Lake is a saline endorheic alkali lake located northwest of Osoyoos in the eastern Similkameen Valley of British Columbia, Canada, accessed via Highway 3. Spotted Lake is richly concentrated with various minerals. It contains dense deposits of magnesium sulfate, calcium and sodium sulphates. It also contains high concentrations of eight other minerals and lower amounts of silver and titanium. Most of the water in the lake evaporates over the summer, revealing colorful mineral deposits. Large “spots” on the lake appear and are colored according to the mineral composition and seasonal amount of precipitation. Magnesium sulfate, which"
"a salinity of 34.8% (i.e. 10 times saltier than ocean water). Probably the best-known hypersaline lakes are the Dead Sea (34.2% salinity in 2010) and the Great Salt Lake in the state of Utah, USA (5–27% variable salinity). The Dead Sea, dividing Israel and the Palestinian West Bank from Jordan, is the world's deepest hypersaline lake and the Araruama Lagoon in Brazil is the world's largest hypersaline lake. The Great Salt Lake, located in Utah, while having nearly three times the surface area of the Dead Sea, is shallower and experiences much greater fluctuations in level than the Dead Sea."
"Spotted Lake Spotted Lake is a saline endorheic alkali lake located northwest of Osoyoos in the eastern Similkameen Valley of British Columbia, Canada, accessed via Highway 3. Spotted Lake is richly concentrated with various minerals. It contains dense deposits of magnesium sulfate, calcium and sodium sulphates. It also contains high concentrations of eight other minerals and lower amounts of silver and titanium. Most of the water in the lake evaporates over the summer, revealing colorful mineral deposits. Large “spots” on the lake appear and are colored according to the mineral composition and seasonal amount of precipitation. Magnesium sulfate, which crystallizes"
"most popular Salt Lake resort until Saltair was built in 1893. The resort was eventually put out of service by a fire in 1904. Great Salt Lake The Great Salt Lake, located in the northern part of the U.S. state of Utah, is the largest salt water lake in the Western Hemisphere, and the eighth-largest terminal lake in the world. In an average year the lake covers an area of around , but the lake's size fluctuates substantially due to its shallowness. For instance, in 1963 it reached its lowest recorded size at 950 square miles (2,460 km²), but in"
"Rewalsar Lake Rewalsar Lake is a mid-altitude lake located on a mountain spur in the Mandi district, 22.5 km south-west from Mandi, in India. Its elevation is about 1,360 m above sea level. The lake is shaped like a square with the shoreline of about 735 m. It is held as a sacred spot for Hindus, Sikhs and Buddhists. There are three Buddhist monasteries at Riwalsar. The lake also has three Hindu temples dedicated to Lord Krishna, Lord Shiva and to the sage Lomas. Another holy lake, Kunt Bhyog which is about 1,750 m above sea level lies above Rewalsar."
"Hypersaline lake A hypersaline lake is a landlocked body of water that contains significant concentrations of sodium chloride or other salts, with saline levels surpassing that of ocean water (3.5%, i.e. ). Specific microbial and crustacean species thrive in these high salinity environments that are inhospitable to most lifeforms. Some of these species enter a dormant state when desiccated, and some species are thought to survive for over 250 million years. The water of hypersaline lakes has great buoyancy due to a high salt content. The most saline water body in the world is the Don Juan Pond, located in"
"(excluding the autonomous regions). Qinghai Lake is the largest salt water lake in China, and the second largest in the world. The Qaidam basin lies in the northwest part of the province. About a third of this resource rich basin is desert. The basin has an altitude between 3000 and 3500 meters. The Sanjiangyuan National Nature Reserve, is located in Qinghai and contains the headwaters of the Yellow River, Yangtze River, and Mekong River. The reserve was established to protect the headwaters of these three rivers and consists of 18 subareas, each containing three zones which are managed with differing"