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Mount Allen Young
Mount Allen Young () is a prominent pyramidal mountain, 2,755 m, standing just south of Fegley Glacier and west of Lennox-King Glacier Lennox-King Glacier is a large valley glacier, about long, draining Bowden Névé and flowing northeast between the Holland Range and the Queen Alexandra Range of Antarctica to enter Richards Inlet, Ross Ice Shelf. It was named by the New Zealand ... in the Holland Range. Discovered by the British Antarctic Expedition (1907–09) and named for Sir Allen Young, polar explorer who led the successful search for Benjamin Leigh Smith in the Arctic in 1882. Mountains of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fegley Glacier
Fegley Glacier () is a tributary glacier in the Holland Range of Antarctica, flowing east into Lennox-King Glacier, northeast of Mount Allen Young. It was named by the Advisory Committee on Antarctic Names for Lieutenant Charles E. Fegley, III, of the Civil Engineer Corps, U.S. Navy, officer in charge of the nuclear power unit at McMurdo Station during Operation Deep Freeze Operation Deep Freeze (OpDFrz or ODF) is codename for a series of United States missions to Antarctica, beginning with "Operation Deep Freeze I" in 1955–56, followed by "Operation Deep Freeze II", "Operation Deep Freeze III", and so on. (There w ..., 1964. References Glaciers of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lennox-King Glacier
Lennox-King Glacier is a large valley glacier, about long, draining Bowden Névé and flowing northeast between the Holland Range and the Queen Alexandra Range of Antarctica to enter Richards Inlet, Ross Ice Shelf. It was named by the New Zealand Geological Survey Antarctic Expedition (1959–60) for Lieutenant Commander James Lennox-King, Royal New Zealand Navy, leader at Scott Base Scott Base is a New Zealand Antarctic research station at Pram Point on Ross Island near Mount Erebus in New Zealand's Ross Dependency territorial claim. It was named in honour of Captain Robert Falcon Scott, RN, leader of two British expedit ..., 1960. See also * Vertigo Bluff References Glaciers of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Holland Range
The Holland Range () is a rugged coastal mountain range in Antarctica, about long, lying just west of the Ross Ice Shelf and extending from Robb Glacier to Lennox-King Glacier. It was named by the Ross Sea Committee for Sir Sidney Holland, who as Prime Minister of New Zealand supported that nation's participation in the Commonwealth Trans-Antarctic Expedition The Commonwealth Trans-Antarctic Expedition (CTAE) of 1955–1958 was a Commonwealth-sponsored expedition that successfully completed the first overland crossing of Antarctica, via the South Pole. It was the first expedition to reach the South ... (1956–58). References Mountain ranges of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nimrod Expedition
The ''Nimrod'' Expedition of 1907–1909, otherwise known as the British Antarctic Expedition, was the first of three successful expeditions to the Antarctic led by Ernest Shackleton and his second expedition to the Antarctic. Its main target, among a range of geographical and scientific objectives, was to be first to the South Pole. This was not attained, but the expedition's southern march reached a Farthest South latitude of 88° 23' S, just from the pole. This was by far the longest southern polar journey to that date and a record convergence on either Pole. A separate group led by Welsh Australian geology professor Edgeworth David reached the estimated location of the South Magnetic Pole, and the expedition also achieved the first ascent of Mount Erebus, Antarctica's second highest volcano. The expedition lacked governmental or institutional support, and relied on private loans and individual contributions. It was beset by financial problems and its preparation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Allen Young
Sir Allen William Young, (12 December 1827 – 20 November 1915) was an English master mariner and explorer, best remembered for his role in Arctic exploration including the search for Sir John Franklin. Early life Allen Young was born at Twickenham on 12 December 1827, and went to sea as a midshipman in the merchant marine in 1842. By 1853 he was master of the Blackwall Frigate ''Marlborough'' and made two round voyages between England and Australia. During the Crimean War, he was master of the 3,000-ton troop ship ''Adelaide''. The ''Fox'' Expeditions In 1857, Allen Young offered himself as sailing master of the auxiliary steamship ''Fox'' under the overall command of Francis Leopold McClintock, that was to search the Franklin expedition, missing since 1845. He also donated 500 pounds to the expedition, and Lady Franklin gratefully accepted his services. The expedition went on to find the only written record of the missing expedition's fate, and Young himself undert ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Benjamin Leigh Smith
Benjamin Leigh Smith (12 March 1828 – 4 January 1913) was an English Arctic explorer and yachtsman. He is the grandson of the Radical abolitionist William Smith. Early life He was born in Whatlington, Sussex, the extramarital child of Anne Longden, a milliner from Alfreton, and the Whig politician Benjamin Smith (1783–1860), the only son of William Smith, a Radical abolitionist. On a visit to his sister in Derbyshire in 1826, Benjamin senior met Anne Longden. She became pregnant by him and he took her to a rented lodge at Whatlington, a small village near Battle, East Sussex. There she lived as "Mrs Leigh", the surname of his relations on the nearby Isle of Wight. The birth of their first child, Barbara Leigh Smith, created a scandal because the couple did not marry, and within eight weeks Anne was pregnant again. When their son Benjamin was born, the four of them went to America for two years, during which time another child was conceived. After their return to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of The Ross Dependency
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
