Mount Westminster
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Mount Westminster
Mount Westminster () is a mountain, 3,370 m, on the east side of Beardmore Glacier, standing 4 nautical miles (7 km) south of Mount Kinsey in the Supporters Range, in Antarctica. Discovered and named by the British Antarctic Expedition (1907–09). Named for Hugh Grosvenor, 2nd Duke of Westminster Hugh Richard Arthur Grosvenor, 2nd Duke of Westminster, (familiarly " Bendor"; 19 March 1879 – 19 July 1953) was a British landowner and one of the wealthiest men in the world. He was the son of Victor Grosvenor, Earl Grosvenor, son of the ..., a financial supporter of the expedition. Mountains of the Ross Dependency Dufek Coast {{DufekCoast-geo-stub ...
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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 (topography), 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 Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, 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 Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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Beardmore Glacier
The Beardmore Glacier in Antarctica is one of the largest valley glaciers in the world, being long and having a width of . It descends about from the Antarctic Plateau to the Ross Ice Shelf and is bordered by the Commonwealth Range of the Queen Maud Mountains on the eastern side and the Queen Alexandra Range of the Central Transantarctic Mountains on the western. The glacier is one of the main passages through the Transantarctic Mountains to the great polar plateau beyond, and was one of the early routes to the South Pole despite its steep upward incline. The glacier was discovered and climbed by Ernest Shackleton during his ''Nimrod'' Expedition of 1908. Although Shackleton turned back at latitude 88° 23' S, just from the South Pole, he established the first proven route towards the pole and, in doing so, became the first person to set foot upon the polar plateau. In 1911–1912, Captain Scott and his ''Terra Nova'' Expedition team reached the South Pole by simi ...
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Mount Kinsey
The Supporters Range () is a rugged range in the Queen Maud Mountains of Antarctica. It is long, bordering the eastern side of Mill Glacier, from Keltie Glacier in the north to Mill Stream Glacier in the south. So named by the New Zealand Geological Survey Antarctic Expedition (NZGSAE) (1961–62) because several peaks of the range are named after supporters of Ernest Shackleton's British Antarctic Expedition (1907–09). Location The northern point of the range lies between Keltie Glacier, flowing from the east, and Mill Glacier flowing from the south and converging with Beardmore Glacier. Ranfurly Point is its northernmost point. Laird Glacier flows from the range in Keltie Glacier, and Snakeskin Glacier flows along the northeast side of the range into Keltie Glacier. Other features in the north include Scully Terrace, Mount Kinsey and Mount Westminster. Features further south include Mount Iveagh, Mount Judd, Mount White and Mount Henry Lucy. The Jensen Glacier flows along the ...
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Supporters Range
The Supporters Range () is a rugged range in the Queen Maud Mountains of Antarctica. It is long, bordering the eastern side of Mill Glacier, from Keltie Glacier in the north to Mill Stream Glacier in the south. So named by the New Zealand Geological Survey Antarctic Expedition (NZGSAE) (1961–62) because several peaks of the range are named after supporters of Ernest Shackleton's British Antarctic Expedition (1907–09). Location The northern point of the range lies between Keltie Glacier, flowing from the east, and Mill Glacier flowing from the south and converging with Beardmore Glacier. Ranfurly Point is its northernmost point. Laird Glacier flows from the range in Keltie Glacier, and Snakeskin Glacier flows along the northeast side of the range into Keltie Glacier. Other features in the north include Scully Terrace, Mount Kinsey and Mount Westminster. Features further south include Mount Iveagh, Mount Judd, Mount White and Mount Henry Lucy. The Jensen Glacier flows along t ...
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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 continent, being about 40% larger than Europe, and has an area of . Most of Antarctica is covered by the Antarctic ice sheet, with an average thickness of . Antarctica is, on average, the coldest, driest, and windiest of the continents, and it has the highest average elevation. It is mainly a polar desert, with annual precipitation of over along the coast and far less inland. About 70% of the world's freshwater reserves are frozen in Antarctica, which, if melted, would raise global sea levels by almost . Antarctica holds the record for the lowest measured temperature on Earth, . The coastal regions can reach temperatures over in summer. Native species of animals include mites, nematodes, penguins, seals and tardigrades. Where vegetation o ...
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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 preparations ...
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Hugh Grosvenor, 2nd Duke Of Westminster
Hugh Richard Arthur Grosvenor, 2nd Duke of Westminster, (familiarly " Bendor"; 19 March 1879 – 19 July 1953) was a British landowner and one of the wealthiest men in the world. He was the son of Victor Grosvenor, Earl Grosvenor, son of the 1st Duke of Westminster, and Lady Sibell Lumley, the daughter of the 9th Earl of Scarborough. Nickname "Bend'Or" From his childhood and during his adult life he was known within family circles as "Bendor", which was also the name of the racehorse Bend Or owned by his grandfather the first Duke, which won The Derby in 1880, the year following his grandson's birth. The name is a jovial reference to the ancient lost armorials of the family: ''Azure, a bend or'', which were awarded to the Scrope family in the famous case of 1389 heard before the Court of Chivalry, known as ''Scrope v Grosvenor''. His wife Loelia wrote in her memoirs: "Of course everybody, even his parents and sisters, would normally have addressed the baby as "Belgrave" so ...
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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 and ...
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