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McCall Point
McCall Point () is a point on the east side of Lallemand Fjord, northwest of Salmon Cove on the west coast of Pernik Peninsula, on the Loubet Coast of Graham Land, Antarctica. It was mapped from air photos taken by the Falkland Islands and Dependencies Aerial Survey Expedition, 1956–57, and was named by the UK Antarctic Place-Names Committee after American engineer John G. McCall (1923–54) of the University of Alaska, who first measured the detailed internal movement of a cirque glacier A cirque glacier is formed in a cirque, a bowl-shaped depression on the side of or near mountains. Snow and ice accumulation in corries often occurs as the result of avalanching from higher surrounding slopes. If a cirque glacier advances far enou ... in 1951–52. References SCAR Composite Gazetteer of Antarctica Headlands of Graham Land Loubet Coast {{LoubetCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lallemand Fjord
The Lallemand Fjord () is a fjord located east of Arrowsmith Peninsula and west of Pernik Peninsula on Loubet Coast on the western side of the Antarctic Peninsula, Antarctica. It begins at Sharp Glacier and runs over 48 km roughly south to north, flowing into Crystal Sound near Detaille Island, and entered between Roux Island and Holdfast Point. The fjord was named by Jean-Baptiste Charcot after the French geographer Charles Lallemand. Stonehouse, Bernard, Encyclopedia of Antarctica and the Southern Oceans, p160 Glaciers Haefeli Glacier, Finsterwalder Glacier, Sharp Glacier, Sölch Glacier, Wilkinson Glacier, Koriten Glacier, Dabrava Glacier Dabrava Glacier ( bg, ледник Дъбрава, lednik Dabrava, ) is the 14 km long and 4.5 km wide glacier on Pernik Peninsula, Loubet Coast in Graham Land, Antarctica Antarctica () is Earth's southernmost and least-populat ..., Brückner Glacier and Antevs Glacier feed the fjord. See also * Shmidt Poi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salmon Cove (Antarctica)
Salmon Cove () is a cove southeast of McCall Point on the east side of Lallemand Fjord in Graham Land. It was mapped by the Falklands Islands Dependencies Survey from surveys and air photos, 1956–59. It was named by the UK 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 ... for Eric M.P. Salmon, an assistant Falklands Islands Dependencies Survey meteorologist who spent several seasons in Antarctica between 1950 and 1956, and visited this cove in 1956. References Bays of Graham Land {{GrahamLand-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pernik Peninsula
Pernik Peninsula ( bg, полуостров Перник, poluostrov Pernik, ) is the ice-covered peninsula projecting 40 km in northwest direction from Loubet Coast on the west side of Antarctic Peninsula. It is bounded by Darbel Bay to the northeast, Lallemand Fjord to the west and Crystal Sound to the northwest, and its northern part is dominated by Protector Heights. The peninsula is named after the city of Pernik in Western Bulgaria. Location Pernik Peninsula is centred at . British mapping in 1976. Maps * British Antarctic Territory. Scale 1:200000 topographic map. DOS 610 Series, Sheet W 66 66. 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 updated. References Bulgarian Antarctic Gazetteer.Antarctic Place-names Commission. (details in Bulgarianbasic datain English) Pernik Peninsula.SCAR Composit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loubet Coast
Loubet Coast is the portion of the west coast of Graham Land in Antarctic Peninsula, extending 158 km between Cape Bellue to the northeast and Bourgeois Fjord to the southwest. South of Loubet Coast is Fallières Coast, north is Graham Coast. The coast is named after Émile Loubet, President of France during the exploration of the area by the French Antarctic Expedition under Jean-Baptiste Charcot in January 1905. Location Loubet Coast is centred at . UK, British mapping in 1976 - 78. Maps * British Antarctic Territory. Scale 1:200000 topographic map. DOS 610 Series, Sheet W 66 64. Directorate of Overseas Surveys, Tolworth, UK, 1976. * British Antarctic Territory. Scale 1:200000 topographic map. DOS 610 Series, Sheet W 66 66. Directorate of Overseas Surveys, Tolworth, UK, 1976. * British Antarctic Territory. Scale 1:200000 topographic map. DOS 610 Series, Sheet W 67 66. Directorate of Overseas Surveys, Tolworth, UK, 1978. References Composite Antarctic Gazetteer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Falkland Islands And Dependencies Aerial Survey Expedition
The Falkland Islands and Dependencies Aerial Survey Expedition (FIDASE) was an aerial survey of the Falkland Islands Dependencies and the Antarctic peninsula which took place in the 1955–56 and 1956–57 southern summers. Funded by the Colonial Office and organized by Peter Mott, the survey was carried out by Hunting Aerosurveys Ltd. The expedition was based at Deception Island and utilized the ''Oluf Sven'', two Canso flying-boats, and several helicopters. The photographic collection, held by the British Antarctic Survey The British Antarctic Survey (BAS) is the United Kingdom's national polar research institute. It has a dual purpose, to conduct polar science, enabling better understanding of global issues, and to provide an active presence in the Antarctic on ... as the United Kingdom Antarctic Mapping Centre, comprises about 12,800 frames taken on 26,700 kilometers of ground track. References {{reflist British Antarctic Territory Surveying of the United Kingdom Pho ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
UK 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 Scientific Committee on Antarctic Research, 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 featu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
John G
John is a common English name and surname: * John (given name) * John (surname) John may also refer to: New Testament Works * Gospel of John, a title often shortened to John * First Epistle of John, often shortened to 1 John * Second Epistle of John, often shortened to 2 John * Third Epistle of John, often shortened to 3 John People * John the Baptist (died c. AD 30), regarded as a prophet and the forerunner of Jesus Christ * John the Apostle (lived c. AD 30), one of the twelve apostles of Jesus * John the Evangelist, assigned author of the Fourth Gospel, once identified with the Apostle * John of Patmos, also known as John the Divine or John the Revelator, the author of the Book of Revelation, once identified with the Apostle * John the Presbyter, a figure either identified with or distinguished from the Apostle, the Evangelist and John of Patmos Other people with the given name Religious figures * John, father of Andrew the Apostle and Saint Peter * Pope Joh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
University Of Alaska
The University of Alaska System is a system of public universities in the U.S. state of Alaska. It was created in 1917 and comprises three separately accredited universities on 19 campuses. The system serves nearly 30,000 full- and part-time students and offers 400 unique degree programs. Each of the three main universities has several satellite campuses in smaller communities. UAA also operates three large satellite community colleges. The three major institutions in the University of Alaska system are: * University of Alaska Anchorage, the largest university by enrollment in the system; * University of Alaska Fairbanks, the first university and flagship; * University of Alaska Southeast, located in the capital city of Juneau, with campuses in Sitka and Ketchikan and the smallest by enrollment. Since the population of Alaska is smaller than that of most U.S. states, the University of Alaska System is a relatively small one. However, it does have several notable academic depart ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cirque Glacier
A cirque glacier is formed in a cirque, a bowl-shaped depression on the side of or near mountains. Snow and ice accumulation in corries often occurs as the result of avalanching from higher surrounding slopes. If a cirque glacier advances far enough, it may become a valley glacier. Additionally, if a valley glacier retreats enough that it is within the cirque, it becomes a cirque glacier again. In these depressions, snow persists through summer months, and becomes glacier ice. Snow may be situated on the leeward slope of a mountain, where it is sheltered from wind. Rock fall from above slopes also plays an important role in sheltering the snow and ice from sunlight. If enough rock falls onto the glacier, it may become a rock glacier. Randklufts may form beneath corrie glaciers as open space between the ice and the bedrock, where meltwater Meltwater is water released by the melting of snow or ice, including glacial ice, tabular icebergs and ice shelves over oceans. Meltwater ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Headlands Of Graham Land
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. Headlands and bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosion of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
