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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 (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 ...
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Lyttelton Peak
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 ...
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Mount Kopere
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 Ne ...
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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. ''The Kon-Tiki Expedition: By Raft Across the South Seas, Kon-Tiki'' is also the name of Heyerdahl's book, the Academy Award for Best Documentary Feature, Academy Award–winning Kon-Tiki (1950 film), 1950 documentary film chronicling his adventures, and the Kon-Tiki (2012 film), 2012 dramatized feature film nominated for the Academy Award for Best Foreign Language Film. Heyerdahl believed that people from South America could have reached Polynesia during pre-Columbian times. His aim in mounting the ''Kon-Tiki'' expedition was to show, by using only the materials and technologies available to those people at the time, that there were no technical reasons to prevent them from having done so. Alth ...
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Cooper Icefalls
The Nimrod Glacier is a major glacier about 135 km (85 mi) long, flowing from the polar plateau in a northerly direction through the Transantarctic Mountains between the Geologists and Miller Ranges, then northeasterly between the Churchill Mountains and Queen Elizabeth Range, and finally spilling 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. See also * List of glaciers in the Antarctic There are many glaciers in the Antarctic. This set of lists does not include ice sheets, ice caps or ice fields, such as the Antarctic ice sheet, but includes glacial features that are defined by their flow, rather than general bodies of ice. Th ... References * External links * Glaciers ...
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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 is associated with 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 days to years depending on freeze-thaw factors. 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 roughly half of the density of liquid water at 1 atm. Névé can also refer to the alpine Alpine may refer to any mountainous region. It may also refer to: Places Europe * Alps, a European mountain range ** Alpine states, which overlap with the European range Australia * Alpine, New South Wales, a Northern Village * Alpine Nati ...
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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,'' which in English is likely to mean "throat" or is otherwise known as the "gullet"; cf. Latin ''gurgulio, gula, gargula'' ("gullet" or "throat") and simila ...
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McMurdo Station
McMurdo Station is a United States Antarctic research station on the south tip of Ross Island, which is in the New Zealand-claimed Ross Dependency on the shore of McMurdo Sound in Antarctica. 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 1,258 residents, and serves as one of three year-round United States Antarctic science facilities. All personnel and cargo going to or coming from Amundsen–Scott South Pole Station first pass through McMurdo. By road, McMurdo is 3 kilometres (1.9 mi) from New Zealand's smaller Scott Base. History The station takes its name from its geographic location on McMurdo Sound, named after Lieutenant Archibald McMurdo of . The ''Terror'', commanded by Irish explorer Francis Crozier, along with expedition flagship ''Erebus'' under command of James Clark Ross, first charted the area ...
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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 presence in the Antarctica continent. Founded in 1959, the USAP manages all U.S. scientific research and related 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, and works with other federal agencies, the U.S. military, an ...
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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 ...
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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 ...
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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 (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 ...
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Charles Lyttelton, 10th Viscount Cobham
Charles John Lyttelton, 10th Viscount Cobham, (8 August 1909 – 20 March 1977) was the 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 is named after their family estate ( Hagley Park, Worcestershire), and the port town of Lyttelton bears his great-grandfather's name. He visited New Zealand in 1950 in relation to property holdings in Christchurch. Military service Lyttel ...
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