- Also called:
- Subglacial Lake Vostok or Lake East
Lake Vostok
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What is Lake Vostok?
Lake Vostok, the largest lake in Antarctica, is located roughly 2.5 miles (4 km) beneath Russiaâs Vostok Station on the East Antarctic Ice Sheet (EAIS). It is the largest known subglacial lake, running more than 150 miles (about 240 km) long with a maximum width of about 31 miles (50 km), and it holds nearly 1,300 cubic miles (5,400 cubic km) of water.
The lake's existence was confirmed in the mid-1990s through seismic and ice-penetrating radar surveys. Scientists believe that volcanic activity melted a portion of the overhead ice to create the lake. A Russian drilling project reached the lake in 2012, and scientists studying the samples reported finding new forms of bacterial life.
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Where is Lake Vostok located?
Lake Vostok, the largest Antarctic lake, lies approximately 2.5 miles (4 km) beneath Russiaâs Vostok Station on the East Antarctic Ice Sheet (EAIS). This subglacial lake stretches over 150 miles (about 240 km) in length and has a maximum width of about 31 miles (50 km). It is roughly elliptical and contains nearly 1,300 cubic miles (5,400 cubic km) of water. The lake's existence was confirmed in the mid-1990s using seismic and ice-penetrating radar surveys. Scientists drilled through 12,366 feet (3,769 meters) of ice to reach the liquid water in February 2012.
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How was Lake Vostok discovered?
The existence of Lake Vostok, the largest Antarctic subglacial lake, was suspected since the 1970s. In the mid-1990s, its existence was confirmed through seismic and ice-penetrating radar surveys conducted by British and Russian researchers. Exact measurements were provided in 1996.
In February 2012, Russian scientists drilled through nearly 2.5 miles (4 km) of ice at Russia's Vostok Station to reach the lake. Pressurized water from the lake rushed up the hole and froze, forming an ice plug. In January 2013, an ice core was removed from the plug and studied.
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Why is Lake Vostok covered by ice?
Lake Vostok, the largest Antarctic lake, is buried under approximately 2.5 miles (4 km) of ice, a phenomenon confirmed in the mid-1990s through seismic and ice-penetrating radar surveys. Most scientists attribute the lake's formation to volcanic activity that melted the overlying ice. Some hypothesize that Lake Vostok has been isolated from Earth's atmosphere since the East Antarctic Ice Sheet (EAIS) formed over 30 million years ago.
In February 2012, a Russian drilling project successfully penetrated 12,366 feet (3,769 meters) of ice to reach the lake's liquid water.
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What makes Lake Vostok unique among the lakes in Antarctica?
Lake Vostok is unique because it is the largest subglacial lake, lying approximately 2.5 miles (4 km) beneath Russiaâs Vostok Station on the East Antarctic Ice Sheet. It is roughly elliptical, with a length of more than 150 miles (240 km) and a maximum width of about 31 miles (50 km), holding nearly 1,300 cubic miles (5,400 cubic km) of water.
Seismic and ice-penetrating radar surveys confirmed its existence in the mid-1990s. Some scientists believe the lake has been isolated from Earthâs atmosphere for over 30 million years, potentially harboring a unique freshwater ecosystem that relies on chemical sources for energy and can withstand extreme pressure. In 2012, researchers drilled through 12,366 feet (3,769 meters) of ice to reach the lake, discovering new forms of bacterial life. Scientists suggest that studying Lake Vostok could help in planning space missions to search for life on ice-covered oceans on other worlds, such as Jupiterâs moon Europa.
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What have scientists learned by studying Lake Vostok?
Lake Vostok, Antarctica's largest subglacial lake, has been the subject of extensive scientific research. Its existence was confirmed in the mid-1990s through seismic and ice-penetrating radar surveys. Scientists believe the lake formed from volcanic activity that melted overlying ice. Drilling into the lake in 2012 allowed scientists to collect samples and data, which led to the discovery of new forms of bacterial life. Some speculate that Lake Vostok may harbor a unique freshwater ecosystem with organisms that have evolved independently from other life forms on Earth. The base of the food chain would need to derive energy from chemical sources rather than photosynthesis, and each organism would need to endure extreme pressure. Scientists suggest that studying Lake Vostok could help in planning future space missions searching for life on ice-covered oceans, such as those on Jupiter's moon Europa.
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Lake Vostok, largest lake in Antarctica. Located approximately 2.5 miles (4 km) beneath Russiaâs Vostok Station on the East Antarctic Ice Sheet (EAIS), the water body is also the largest subglacial lake known. Running more than 150 miles (about 240 km) long with a maximum width of about 31 miles (50 km), the lake is roughly elliptical in shape, and it holds nearly 1,300 cubic miles (5,400 cubic km) of water. After decades of speculation and data gathering, the existence of the lake was confirmed in the mid-1990s by a combination of seismic and ice-penetrating radar surveys.
Most scientists believe that the lake is the product of volcanic activity that melted a portion of the ice overhead. Some scientists maintain that the lake was isolated from Earthâs atmosphere after the EAIS formed more than 30 million years ago. Other scientists argue that the water making up the lake may be much younger, perhaps only about 400,000 years old. Most scientists, however, agree that Lake Vostok might harbor a unique freshwater ecosystem made up of organisms that evolved independently from other forms of life on Earth. The base of the lakeâs food chain would need to derive its energy from chemical sources rather than from photosynthesis, and each organism in this environment would need to endure the pressure of 350 atmospheres (about 5,150 pounds per square inch) brought on by the weight of ice sheet above.
A Russian drilling project designed to retrieve ice cores below Vostok Station was initiated in 1990; the station was later found to sit directly above the lake. After the lakeâs existence was revealed, the scientists continued to drill, ultimately penetrating some 12,366 feet (3,769 meters) of ice in February 2012 to reach liquid water. Worries over possible contamination of the lake from the drillâas well as the freeze-resistant fluids, such as Freon and kerosene, used in the drilling processâwere dispelled when the drill tip punched through the final layers of ice. Pressurized water from the lake rushed up the hole, which forced the drilling fluids upward and away from the lake, before freezing into a 100â130-foot- (30â40-meter-) long ice plug. Shortly after the drill reached the plug, however, the scientists left the station to escape the onset of the coldest part of the Antarctic winter. An ice core was removed from the plug in January 2013 and studied by a Russian team of scientists. In March of that year, after preliminary analyses of the samples taken from the ice core had been completed, Russian state media announced that evidence of bacterial DNA had been found, including at least one type that did not correspond to bacteria known to science. This discovery, however, was later called into question because of possible sample contamination.
Several scientists have remarked that the effort to reach Lake Vostok could be a valuable planning and implementation tool for future space missions designed to search for life on worlds containing ice-covered oceans, such as those that occur on Jupiterâs moon Europa.