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Spermwhale Ridge
Spermwhale Ridge () is a sharp-crested ridge rising to about 800 m in northern Voden Heights and flanking the south side of Flask Glacier west of Bulkington Pass, on Oscar II Coast, Graham Land. Named by the United Kingdom Antarctic Place-Names Committee The UK Antarctic Place-Names Committee (or UK-APC) is a United Kingdom government committee, part of the Foreign and Commonwealth Office, responsible for recommending names of geographical locations within the British Antarctic Territory (BAT) and ... (UK-APC) in 1987. One of several names in this area from Melville's Moby Dick, reflecting a whaling theme. Ridges of Graham Land Oscar II Coast Place names inspired by Moby-Dick {{OscarIICoast-geo-stub ...
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Voden Heights
Voden Heights ( bg, Воденски възвишения, ‘Vodenski Vazvisheniya’ \'vo-den-ski v&z-vi-'she-ni-ya\) are the heights extending 42.5 km in the east-west direction and 15.4 km wide, rising to 1700 m ( Mount Zadruga) on Oscar II Coast in Graham Land. They are bounded by Flask Glacier to the north, Scar Inlet to the east, Leppard Glacier to the south and its tributary Fleece Glacier to the southwest, and linked by a wide ice-covered saddle to Bruce Plateau to the west. The feature is named after the settlements of Voden in Northeastern, Southeastern, and Southern Bulgaria. Location Voden Heights are centred at . British mapping in 1976. Maps * British Antarctic Territory. Scale 1:200000 topographic map. DOS 610 Series, Sheet W 65 62. Directorate of Overseas Surveys, Tolworth, UK, 1976. Antarctic Digital Database (ADD).Scale 1:250000 topographic map of Antarctica. Scientific Committee on Antarctic Research (SCAR). Since 1993, regularly upgraded and up ...
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Flask Glacier
Flask Glacier (), is a gently-sloping glacier, long, flowing east from Bruce Plateau to enter Scar Inlet between Daggoo Peak and Spouter Peak in Graham Land, Antarctica. The lower reaches of this glacier were surveyed and photographed by the Falklands Islands Dependencies Survey (FIDS) in 1947. The entire glacier was photographed by the Falkland Islands and Dependencies Aerial Survey Expedition in 1955–56, and mapped by the FIDS in 1957. It was named by the UK Antarctic Place-names Committee after the third mate on the ''Pequod'' in Herman Melville's '' Moby-Dick; or, The White Whale''. Tributary glaciers * Ambergris Glacier * Belogradchik Glacier See also * List of glaciers in the Antarctic * List of Antarctic ice streams * Glaciology Further reading * T. A. Scambos, J. A. Bohlander, C. A. Shuman, P. Skvarca, https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2004GL020670 Glacier acceleration and thinning after ice shelf collapse in the Larsen B embayment, An ...
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Bulkington Pass
Bulkington Pass () is a pass on the south side of Flask Glacier and west of Bildad Peak in Voden Heights on the east side of Graham Land. The pass trends northeast–southwest for and provides a route from the ice piedmont north of Adit Nunatak to Flask Glacier. The toponym is one in a group applied by the UK Antarctic Place-Names Committee that reflects a whaling theme, Bulkington being a crewman on the vessel ''Pequod'' in Herman Melville Herman Melville (Name change, born Melvill; August 1, 1819 – September 28, 1891) was an American people, American novelist, short story writer, and poet of the American Renaissance (literature), American Renaissance period. Among his bes ...'s Moby Dick. References Mountain passes of Graham Land Oscar II Coast Place names inspired by Moby-Dick {{OscarIICoast-geo-stub ...
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Oscar II Coast
Oscar II Coast is that portion of the east coast of the Antarctic Peninsula between Cape Fairweather to the north, and Cape Alexander to the south. Discovered in 1893 by Captain C.A. Larsen, who named it for King Oscar II of Norway and Sweden. To the north of this coast is Nordenskjöld Coast The Nordenskjöld Coast (64° 30' S 60° 30' W) is located on the Antarctic Peninsula, more specifically Graham Land, which is the top region of the Peninsula. The Peninsula is a thin, long ice sheet with an Alpine-style mountain chain. The coast .... Further reading * Alan Nairn, 'The South Atlantic, Volume 1'', P 192 * Gunter Faure, Teresa M. Mensing, 'The Transantarctic Mountains: Rocks, Ice, Meteorites and Water'', P 9 * R. L. Oliver, P. R. James, J. B. Jago, 'Antarctic Earth Science'', P 329 * Amin Beiranvand Pour, Mazlan Hashim, Yongcheol Park and Jong Kuk Hong, 'MAPPING ALTERATION ZONES IN INACCESSIBLE REGIONS USING TARGET DETECTION ALGORITHMS TO SWIR BANDS OF ASTER REMOTE SENS ...
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Graham Land
Graham Land is the portion of the Antarctic Peninsula that lies north of a line joining Cape Jeremy and Cape Agassiz. This description of Graham Land is consistent with the 1964 agreement between the British Antarctic Place-names Committee and the US Advisory Committee on Antarctic Names, in which the name "Antarctic Peninsula" was approved for the major peninsula of Antarctica, and the names Graham Land and Palmer Land for the northern and southern portions, respectively. The line dividing them is roughly 69 degrees south. Graham Land is named after Sir James R. G. Graham, First Lord of the Admiralty at the time of John Biscoe's exploration of the west side of Graham Land in 1832. It is claimed by Argentina (as part of Argentine Antarctica), Britain (as part of the British Antarctic Territory) and Chile (as part of the Chilean Antarctic Territory). Graham Land is the closest part of Antarctica to South America. Thus it is the usual destination for small ships taking paying ...
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United Kingdom Antarctic Place-Names Committee
The UK Antarctic Place-Names Committee (or UK-APC) is a United Kingdom government committee, part of the Foreign and Commonwealth Office, responsible for recommending names of geographical locations within the British Antarctic Territory (BAT) and the South Georgia and the South Sandwich Islands (SGSSI). Such names are formally approved by the Commissioners of the BAT and SGSSI respectively, and published in the BAT Gazetteer and the SGSSI Gazetteer maintained by the Committee. The BAT names are also published in the international Composite Gazetteer of Antarctica maintained by SCAR. The Committee may also consider proposals for new place names for geographical features in areas of Antarctica outside BAT and SGSSI, which are referred to other Antarctic place-naming authorities, or decided by the Committee itself if situated in the unclaimed sector of Antarctica. Names attributed by the committee * Anvil Crag, named for descriptive features * Anckorn Nunataks, named after J. F. ...
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Moby Dick
''Moby-Dick; or, The Whale'' is an 1851 novel by American writer Herman Melville. The book is the sailor Ishmael's narrative of the obsessive quest of Ahab, captain of the whaling ship ''Pequod'', for revenge against Moby Dick, the giant white sperm whale that on the ship's previous voyage bit off Ahab's leg at the knee. A contribution to the literature of the American Renaissance, ''Moby-Dick'' was published to mixed reviews, was a commercial failure, and was out of print at the time of the author's death in 1891. Its reputation as a " Great American Novel" was established only in the 20th century, after the 1919 centennial of its author's birth. William Faulkner said he wished he had written the book himself, and D. H. Lawrence called it "one of the strangest and most wonderful books in the world" and "the greatest book of the sea ever written". Its opening sentence, "Call me Ishmael", is among world literature's most famous. Melville began writing ''Moby-Dick'' in February ...
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Ridges Of Graham Land
A ridge or a mountain ridge is a geographical feature consisting of a chain of mountains or hills that form a continuous elevated crest for an extended distance. The sides of the ridge slope away from the narrow top on either side. The lines along the crest formed by the highest points, with the terrain dropping down on either side, are called the ridgelines. Ridges are usually termed hills or mountains as well, depending on size. Smaller ridges, especially those leaving a larger ridge, are often referred to as spurs. Types There are several main types of ridges: ;Dendritic ridge: In typical dissected plateau terrain, the stream drainage valleys will leave intervening ridges. These are by far the most common ridges. These ridges usually represent slightly more erosion resistant rock, but not always – they often remain because there were more joints where the valleys formed or other chance occurrences. This type of ridge is generally somewhat random in orientation, often ...
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