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Tarakanov Ridge
The Cobham Range () is a mountain range in the Churchill Mountains of the Ross Dependency, Antarctica. It extends to the north of the Nimrod Glacier. Location The Cobham Range trends in a northwest–southeast direction for about in the southern part of the Churchill Mountains of the Ross Dependency, Antarctica. The Prince Philip Glacier runs south down the east side of the Cobham Range, and the Lucy Glacier runs southeast down the west side. They both feed the Nimrod Glacier, which flows to the northeast past the south end of the range. The Holyoake Range is east of the Cobham Range on the east side of the Prince Philip Glacier. The Queen Elizabeth Range (Antarctica), Queen Elizabeth Range is south of the Cobham Range on the south side of the Nimrod Glacier. Early exploration and naming The Cobham Range was mapped by the northern party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1961–62, and named by the New Zealand Antarctic Place-Names Committee fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kon-Tiki
The ''Kon-Tiki'' expedition was a 1947 journey by raft across the Pacific Ocean from South America to the Polynesian islands, led by Norwegian explorer and writer Thor Heyerdahl. The raft was named ''Kon-Tiki'' after the Inca god Viracocha, for whom "Kon-Tiki" was said to be an old name. Heyerdahl's book on the expedition was entitled '' The Kon-Tiki Expedition: By Raft Across the South Seas''. A 1950 documentary film won the Academy Award for Best Documentary Feature. A 2012 dramatized feature film was nominated for the Academy Award for Best Foreign Language Film. The ''Kon-Tiki'' expedition was funded by private loans, along with donations of equipment from the United States Army. Heyerdahl and a small team went to Peru, where, with the help of dockyard facilities provided by the Peruvian authorities, they constructed the raft out of balsa logs and other native materials in an indigenous style as recorded in illustrations by Spanish conquistadores. The trip began on A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cooper Icefalls
The Nimrod Glacier () is a major glacier about long, flowing from the polar plateau in a northerly direction through the Transantarctic Mountains into the Ross Ice Shelf, Antarctica. Location The Nimrod Glacier flows north between the Geologists and Miller Ranges, then northeasterly between the Churchill Mountains and Queen Elizabeth Range, and finally spills into Shackleton Inlet and the Ross Ice Shelf between Capes Wilson and Lyttelton. It was photographed from the air by USN Operation Highjump, 1946–47. The name, given by US-ACAN, is in association with Shackleton Inlet and is for the ''Nimrod'', the ship of the British Antarctic Expedition (1907–09) under Ernest Shackleton. The mouth of the glacier is southeast of the Starshot Glacier and the Nursery Glacier. It is north of Robb Glacier. Icefalls Worsley Icefalls Icefalls near the head of Nimrod Glacier. Seen by the northern party of the NZGSAE (1961-62) and presumbably named for Frank Worsley, member of the Bri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Névé
Névé is a young, granular type of snow which has been partially melted, refrozen and compacted, yet precedes the form of ice. This type of snow can contribute to glacier formation through the process of ''nivation''. Névé that survives a full season of ablation turns into firn, which is both older and slightly denser. Firn eventually becomes glacial ice – the long-lived, compacted ice that glaciers are composed of. Glacier formation can take years to hundreds of years, depending on freeze-thaw factors and snow-compaction rates. Névé is annually observed in skiing slopes, and is generally disliked as an icy falling zone. Névé has a minimum density of 500 kg/m3, which is Density#Water, roughly half of the density of liquid water at 1 Atmosphere (unit), atm. Névé can also refer to the Alpine climate, alpine region in which snowfall accumulates, becomes névé, and feeds a glacier. See also * Suncup (snow), Suncup Notes External links * Névés, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gargoyle Ridge In The McMurdo Dry Valleys In Antarctica (30877661786)
In architecture, and specifically Gothic architecture, a gargoyle () is a carved or formed grotesque with a spout designed to convey water from a roof and away from the side of a building, thereby preventing it from running down masonry walls and eroding the mortar between. Architects often used multiple gargoyles on a building to divide the flow of rainwater off the roof to minimize potential damage from rainstorms. A trough is cut in the back of the gargoyle and rainwater typically exits through the open mouth. Gargoyles are usually elongated fantastical animals because their length determines how far water is directed from the wall. When Gothic flying buttresses were used, aqueducts were sometimes cut into the buttress to divert water over the aisle walls. Etymology The term originates from the French ''gargouille'' (Old French ''gargoule'' (1294) "conduit for waterflow"), composed of the onomatopoeic root ''garg-'' and the Old French ''goule'' "animal mouth, throat", whi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
McMurdo Station
McMurdo Station is an American Antarctic research station on the southern tip of Ross Island. It is operated by the United States through the United States Antarctic Program (USAP), a branch of the National Science Foundation. The station is the largest community in Antarctica, capable of supporting up to 1,500 residents, though the population fluctuates seasonally; during the antarctic night, there are fewer than two hundred people. It serves as one of three year-round United States Antarctic science facilities. Personnel and cargo going to or coming from Amundsen–Scott South Pole Station usually first pass through McMurdo, either by flight or by the McMurdo to South Pole Traverse; it is a hub for activities and science projects in Antarctica. McMurdo, Amundsen-Scott, and Palmer are the three non-seasonal United States stations on the continent, though by the Antarctic Treaty System the bases are not a legal claim (though the right is not forfeited); they are dedicated to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
United States Antarctic Program
The United States Antarctic Program (or USAP; formerly known as the United States Antarctic Research Program or USARP and the United States Antarctic Service or USAS) is an organization of the United States government which has a presence in the Antarctica continent. Founded in 1959, the USAP manages all U.S. Research stations in Antarctica, scientific research and related Transport in Antarctica, logistics in Antarctica as well as aboard ships in the Southern Ocean. United States Antarctic Program The United States established the U.S. Antarctic Research Program (USARP) in 1959—the name was later changed to the U.S. Antarctic Program—immediately following the success of the International Geophysical Year (IGY). Today, the National Science Foundation (NSF) has a Presidential Mandate to manage the United States Antarctic Program, through which it operates three year-round research stations and two research vessels, coordinates all U.S. science on the southernmost continent, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Advisory Committee On Antarctic Names
The Advisory Committee on Antarctic Names (ACAN or US-ACAN) is an advisory committee of the United States Board on Geographic Names responsible for recommending commemorative names for features in Antarctica. History The committee was established in 1943 as the Special Committee on Antarctic Names (SCAN). It became the Advisory Committee on Antarctic Names in 1947. Fred G. Alberts was Secretary of the Committee from 1949 to 1980. By 1959, a structured nomenclature was reached, allowing for further exploration, structured mapping of the region and a unique naming system. A 1990 ACAN gazeeter of Antarctica listed 16,000 names. Description The United States does not recognise territorial boundaries within Antarctica, so ACAN assigns names to features anywhere within the continent, in consultation with other national nomenclature bodies where appropriate, as defined by the Antarctic Treaty System. The research and staff support for the ACAN is provided by the United States Geologi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
C82195s1 Ant
C8, C08, C.VIII or C-8 may refer to: Transportation Aviation * AEG C.VIII, a World War I German armed reconnaissance aircraft * AGO C.VIII, a World War I German reconnaissance aircraft * Cierva C.8, a 1926 Spanish experimental autogyro * De Havilland Canada C-8 Buffalo, a military transport aircraft of the 1960s * Fairchild C-8, a military transport aircraft of the 1930s * Fokker C.VIII, a 1928 Dutch reconnaissance aircraft * Chicago Express Airlines (defunct) IATA code Automotive * Citroën C8, a brand of minivan * Sauber C8, a 1985 racing car * Spyker C8, a sportscar produced by car manufacturer Spyker Cars * Eighth generation Chevrolet Corvette (C8) Nautical * HMS ''C8'', a 1907 C-class submarine of the Royal Navy * USS ''Raleigh'' (C-8), an 1892 protected cruiser of the United States Navy Rail * LSWR C8 class, a London and South Western Railway locomotive class * C-8 (Cercanías Madrid) * LNER Class C8, a class of 2 4-cylinder compound locomotives ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gargoyle Ridge
The Cobham Range () is a mountain range in the Churchill Mountains of the Ross Dependency, Antarctica. It extends to the north of the Nimrod Glacier. Location The Cobham Range trends in a northwest–southeast direction for about in the southern part of the Churchill Mountains of the Ross Dependency, Antarctica. The Prince Philip Glacier runs south down the east side of the Cobham Range, and the Lucy Glacier runs southeast down the west side. They both feed the Nimrod Glacier, which flows to the northeast past the south end of the range. The Holyoake Range is east of the Cobham Range on the east side of the Prince Philip Glacier. The Queen Elizabeth Range is south of the Cobham Range on the south side of the Nimrod Glacier. Early exploration and naming The Cobham Range was mapped by the northern party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1961–62, and named by the New Zealand Antarctic Place-Names Committee for a former Governor-General of New ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Charles Lyttelton, 10th Viscount Cobham
Charles John Lyttelton, 10th Viscount Cobham (8 August 1909 – 20 March 1977) was the List of Governors-General of New Zealand, ninth Governor-General of New Zealand and an English cricketer from the Lyttelton family. Background and education Lyttelton was born in Kensington, London, the son of John Lyttelton, 9th Viscount Cobham, and Violet Yolande Leonard. He was a cousin of the musician Humphrey Lyttelton. He was educated at Eton College and Trinity College, Cambridge, graduating with a law degree in 1932. He had a family connection with New Zealand, where he became governor-general, through his great-grandfather George Lyttelton, 4th Baron Lyttelton, who was chairman of the Canterbury Association and contributed financially to the early development of Christchurch. Hagley Park, Christchurch, Hagley Park is named after their family estate (Hagley Park, Worcestershire), and the port town of Lyttelton, New Zealand, Lyttelton bears his great-grandfather's name. He visited New Ze ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
