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Pain Neve
Pain Neve () is a neve between Commonwealth Range and Hughes Range from which the Keltie Glacier drains southwestward to enter Beardmore Glacier. Named by the Southern Party of New Zealand Geological Survey Antarctic Expedition (NZGSAE) (1961–62) for Kevin Pain Kevin () is the anglicized form of the Irish masculine given name (; mga, CaoimhghÃn ; sga, Cóemgein ; Latinized as ). It is composed of "dear; noble"; Old Irish and ("birth"; Old Irish ). The variant '' Kevan'' is anglicized from , a ..., field assistant with the party. Snow fields of the Ross Dependency Dufek Coast {{DufekCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Commonwealth Range
The Commonwealth Range is a north-south trending range of rugged mountains, long, located within the Queen Maud Mountains on the Dufek Coast of the continent of Antarctica. The range borders the eastern side of Beardmore Glacier from the Ross Ice Shelf to Keltie Glacier. The range was discovered by the British Antarctic Expedition (1907–09) and named by the expedition after the Commonwealth of Australia, which gave much assistance to the expedition. Key features Its highest peak is Flat Top at 4000 meters or 13,123 feet. Other peaks within the range include: * |
Hughes Range (Antarctica)
The Hughes Range is a high massive north–south trending mountain range in Antarctica, surmounted by six prominent summits, of which Mount Kaplan (4,230 m) is the highest. The range is located east of Canyon Glacier in the Queen Maud Mountains and extends from the confluence of Brandau and Keltie glaciers in the south, to the Giovinco Ice Piedmont in the north. Discovered and photographed by Rear Admiral Byrd on the baselaying flight of November 18, 1929, and named by the Advisory Committee on Antarctic Names on the recommendation of Byrd for Charles Evans Hughes, U.S. secretary of state, U.S. chief justice, and adviser/counselor of Byrd. Key mountains *Mount Kaplan *Mount Waterman () is a massive mountain, , standing NE of Mount Wexler. The mountain was discovered and photographed by Rear Admiral Byrd on the baselaying flight of November 18, 1929, and surveyed by A.P. Crary from 1957 to 1958. Named by Crary for Alan Tower Waterman, director of the National Science Foundation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Keltie Glacier
Keltie Glacier is a large Antarctic glacier, long, draining from Pain Névé southwest around the southern extremity of the Commonwealth Range, and then northwest to enter Beardmore Glacier at Ranfurly Point. It was discovered by the British Antarctic Expedition, 1907–09, under Ernest Shackleton, who named it for Sir John Scott Keltie Sir John Scott Keltie (29 March 1840 – 12 January 1927) was a Scottish geographer, best known for his work with the Royal Geographical Society. History Keltie was born in Dundee and attended school in Perth. He matriculated at the Unive ..., Secretary of the Royal Geographical Society, 1892–1915. See also * List of glaciers in the Antarctic References Glaciers of Dufek Coast Queen Maud Mountains {{DufekCoast-glacier-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southern Party (New Zealand Geological Survey Antarctic Expedition)
The Southern Party (SP) was a minor political party in the United States American electoral politics have been dominated by two major political parties since shortly after the founding of the republic of the United States of America. Since the 1850s, the two have been the Democratic Party and the Republican Party†... that operated exclusively in the South. The party supported states' rights and increased Southern cultural and regionalist activism. The party was formed by the League of the South in 1999 and experienced moderate success following the framing of the Asheville Declaration, which was touted by the party as a second United States Declaration of Independence, Declaration of Independence. Despite its initial success, the Southern Party was disbanded in 2003 following internal factionalism; all that exists of the Southern Party today are the remnants of its state chapters in Florida, Georgia (U.S. state), Georgia, North Carolina, and Mississippi. History The mer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand Geological Survey Antarctic Expedition
The New Zealand Geological Survey Antarctic Expedition (NZGSAE) describes a series of scientific explorations of the continent Antarctica. The expeditions were notably active throughout the 1950s and 1960s. Features named by the expeditions 1957–1958 expedition The 1957–1958 expedition went to the Ross Dependency and named the Borchgrevink Glacier. Other features named include: * Carter Ridge * Felsite Island * Halfway Nunatak * Hedgehog Island * Moraine Ridge 1958–1959 expedition * Cadwalader Beach * Cape Hodgson * Carter Ridge * Isolation Point * Mountaineer Range * Mount Aurora * Mount Hayward * Mount Henderson (White Island) * Mount Bird. 1960–1961 expedition * Deverall Island * Lonewolf Nunataks 1961–1962 expedition * Aurora Heights * The Boil * Ford Spur * Graphite Peak * Half Century Nunatak * Half Dome Nunatak * Hump Passage * Last Cache Nunatak * Lookout Dome * Montgomerie Glacier * Mount Fyfe * Mount Macdonald * Snowshoe Pass * Turret Nu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kevin Pain
Kevin () is the anglicized form of the Irish masculine given name (; mga, CaoimhghÃn ; sga, Cóemgein ; Latinized as ). It is composed of "dear; noble"; Old Irish and ("birth"; Old Irish ). The variant ''Kevan'' is anglicized from , an Irish diminutive form.''A Dictionary of First Names''. Oxford University Press (2007) s.v. "Kevin". The feminine version of the name is (anglicised as ''Keeva'' or ''Kweeva''). History Saint Kevin (d. 618) founded Glendalough abbey in the Kingdom of Leinster in 6th-century Ireland. Canonized in 1903, he is one of the patron saints of the Archdiocese of Dublin. Caomhán of Inisheer, the patron saint of Inisheer, Aran Islands, is properly anglicized ''Cavan'' or ''Kevan'', but often also referred to as "Kevin". The name was rarely given before the 20th century. In Ireland an early bearer of the anglicised name was Kevin Izod O'Doherty (1823–1905) a Young Irelander and politician; it gained popularity from the Gaelic revival of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Snow Fields Of The Ross Dependency
Snow comprises individual ice crystals that grow while suspended in the atmosphere—usually within clouds—and then fall, accumulating on the ground where they undergo further changes. It consists of frozen crystalline water throughout its life cycle, starting when, under suitable conditions, the ice crystals form in the atmosphere, increase to millimeter size, precipitate and accumulate on surfaces, then metamorphose in place, and ultimately melt, slide or Sublimation (phase transition), sublimate away. Snowstorms organize and develop by feeding on sources of atmospheric moisture and cold air. Snowflakes Nucleation, nucleate around particles in the atmosphere by attracting supercooling, supercooled water droplets, which Freezing, freeze in hexagonal-shaped crystals. Snowflakes take on a variety of shapes, basic among these are platelets, needles, columns and Hard rime, rime. As snow accumulates into a snowpack, it may blow into drifts. Over time, accumulated snow metamo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
