Hart Glacier (Antarctica)
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The Wright Valley, named for Sir Charles Wright, is the central one of the three large
Dry Valleys The McMurdo Dry Valleys are a row of largely snow-free valleys in Antarctica, located within Victoria Land west of McMurdo Sound. The Dry Valleys experience extremely low humidity and surrounding mountains prevent the flow of ice from nearby ...
in the Transantarctic Mountains, located west of McMurdo Sound at approximately . Wright Valley contains the
Onyx River The Onyx River is an Antarctic meltwater stream which flows westward through the Wright Valley from Wright Lower Glacier and Lake Brownworth at the foot of the glacier to Lake Vanda, during the few months of the Antarctic summer. At in length ...
, the longest river in
Antarctica Antarctica () is Earth's southernmost and least-populated continent. Situated almost entirely south of the Antarctic Circle and surrounded by the Southern Ocean, it contains the geographic South Pole. Antarctica is the fifth-largest contine ...
,
Lake Brownworth Lake Brownworth is a meltwater lake immediately west of Wright Lower Glacier at the east end of Wright Valley, Victoria Land. The lake was mapped by the United States Geological Survey (USGS) from surveys and air photos obtained in 1956–1960. It ...
, the origin of the Onyx River, and Lake Vanda, which is fed by the Onyx River. Its southwestern branch, ''South Fork'', is the location of
Don Juan Pond Don Juan Pond is a small and very shallow hypersaline lake in the western end of Wright Valley (South Fork), Victoria Land, Antarctica, west from Lake Vanda. It is wedged between the Asgard Range to the south and the Dais Range to the north. On t ...
. The upland area known as the
Labyrinth In Greek mythology, the Labyrinth (, ) was an elaborate, confusing structure designed and built by the legendary artificer Daedalus for King Minos of Crete at Knossos. Its function was to hold the Minotaur, the monster eventually killed by the ...
is at the valley's west end. Although portions of the interconnected valley system were discovered in 1903 by the ''Discovery'' expedition led by Captain Robert Falcon Scott, the Wright Valley located near the centre of the system was not seen until aerial photographs of the region were made in 1947. By the mid 1960s scientists were becoming increasingly intrigued by the paradoxical fact that the valley lay immediately adjacent to the permanent East Antarctic Ice Sheet, yet had remained ice-free for at least thousands of years. Although Lake Vanda is covered by roughly of ice year-round, lake temperatures of had been reliably measured at a depth of .Ragotzkie, R. A., and G. Likens, 1964: "The heat balance of two Antarctic lakes." ''Limnology and Oceanography'' 9, 412-425 (abstract available onlin
here
Increasing summer field activity and a clear need to establish a winter record led New Zealand's Antarctic Division and the
National Science Foundation The National Science Foundation (NSF) is an independent agency of the United States government that supports fundamental research and education in all the non-medical fields of science and engineering. Its medical counterpart is the National I ...
of the United States to plan a more permanent base in the valley. In 1968 New Zealand established
Vanda Station Vanda Station was an Antarctic research base in the western highlands (Victoria Land) of the Ross Dependency, specifically on the shore of Lake Vanda, at the mouth of Onyx River, in the Wright Valley. History The four original station buildings ...
near the eastern end of Lake Vanda. Martin Cirque occupies the south wall of Wright Valley between Denton Glacier and Nichols Ridge.


See also

* Connell Pond * Headwall Pond * Lake Bull * Dry Valleys Geology * Sarcophagus Pond * Taylor Valley (south) * Victoria Valley (north)


References


External links


Wright Valley panoramic picture, view from Dais intrusion
Valleys of Victoria Land McMurdo Dry Valleys Transantarctic Mountains {{McMurdoDryValleys-geo-stub