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Caution Point
Caution Point () is a headland northeast of Mount Birks, on the north side of the entrance to Spillane Fjord, which marks the east end of Austa Ridge that forms the north wall of Crane Glacier, on the east coast of Graham Land. It was photographed from the air by Sir Hubert Wilkins on a flight of December 20, 1928, and named by the Falkland Islands Dependencies 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 ... who charted it in 1947. References Headlands of Graham Land Oscar II Coast {{OscarIICoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Birks
Mount Birks () is a conspicuous, pyramid-shaped mountain rising to 1,035 m in Austa Ridge on Oscar II Coast in Graham Land, and surmounting Spillane Fjord to the south and Veselie Glacier to the north. In 1928 Sir Hubert Wilkins gave the name Mount Napier Birks, after Napier Birks of Adelaide, Australia, to two conspicuous, black peaks which he observed and photographed from the air as lying close north of his Crane Channel. This coast was charted by the Falkland Islands Dependencies Survey (FIDS) in 1947, but it has not been possible to identify Wilkins' Mount Napier Birks. Since Crane Channel was definitely identified as Crane Glacier, 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) recommended in 1950 that the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spillane Fjord
Spillane Fjord is a fjord in front of Crane Glacier in the western part of Exasperation Inlet, Oscar II Coast in Graham Land, entered between Caution Point and Delusion Point. The feature is 2 miles wide, 10 miles long and averages 1000 m deep. Its greatest depth is 1250 m at the far west end of the fjord. The fjord was created by the catastrophic retreat of Crane Glacier, which was itself caused by the breakup of the north portion of the Larsen Ice Shelf in March, 2002. The fjord's creation was documented by satellite images and the feature was first visited by surface ship in April 2006 during the U.S. Antarctic Program NBP06-03 cruise, when the extent, depth and dimension were determined by swath bathymetry. Named by US-ACAN in 2007 after Joshua Spillane who served the USAP as a marine technician aboard L.M. Gould and N.B. Palmer. He lost his life in Drake Passage, April 16, 2006, while L.M. Gould was transiting from Palmer Station to Punta Arenas, Chile. Location Spillane ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Austa Ridge
Austa Ridge ( bg, italic=yes, хребет Ауста, ‘Hrebet Austa’ \'hre-bet a-'us-ta\) is the partly ice-free ridge extending 24 km and 11 km wide on Oscar II Coast in Graham Land descending eastwards from the south extremity of Forbidden Plateau towards Caution Point. It rises to over 1800 mReference Elevation Model of Antarctica. Polar Geospatial Center. University of Minnesota, 2019 at its west extremity, and surmounts and Borima Bay to the north, |
Crane Glacier
Crane Glacier (), is a narrow glacier which flows in an east-northeasterly direction along the northwest side of Aristotle Mountains to enter Spillane Fjord south of Devetaki Peak, on the east coast of the Antarctic Peninsula. Sir Hubert Wilkins photographed this feature from the air in 1928 and gave it the name "Crane Channel", after C.K. Crane of Los Angeles, reporting that it appeared to be a channel cutting in an east-west direction across the peninsula. The name was altered to "Crane Inlet" following explorations along the west coast of the peninsula in 1936 by the British Graham Land Expedition, which proved that no through channel from the east coast existed as indicated by Wilkins. Comparison of Wilkins' photograph of this feature with those taken in 1947 by the Falklands Islands Dependencies Survey shows that Wilkins' "Crane Channel" is this glacier, although it lies about northeast of the position originally reported by Wilkins. The speed of Crane Glacier increase ... [...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 pay ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sir Hubert Wilkins
Sir George Hubert Wilkins MC & Bar (31 October 188830 November 1958), commonly referred to as Captain Wilkins, was an Australian polar explorer, ornithologist, pilot, soldier, geographer and photographer. He was awarded the Military Cross after he assumed command of a group of American soldiers who had lost their officers during the Battle of the Hindenburg Line, and became the only official Australian photographer from any war to receive a combat medal. He narrowly failed in an attempt to be the first to cross under the North Pole in a submarine, but was able to prove that submarines were capable of operating beneath the polar ice cap, thereby paving the way for future successful missions. The US Navy later took his ashes to the North Pole aboard the submarine USS ''Skate'' on 17 March 1959. Early life Hubert Wilkins was a native of Mount Bryan East, South Australia, the last of 13 children in a family of pioneer settlers and sheep farmers. He was born at Mount Bryan East ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Falkland Islands Dependencies 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 behalf of the UK. It is part of the Natural Environment Research Council (NERC). With over 400 staff, BAS takes an active role in Antarctic affairs, operating five research stations, one ship and five aircraft in both polar regions, as well as addressing key global and regional issues. This involves joint research projects with over 40 UK universities and more than 120 national and international collaborations. Having taken shape from activities during World War II, it was known as the Falkland Islands Dependencies Survey until 1962. History Operation Tabarin was a small British expedition in 1943 to establish permanently occupied bases in the Antarctic. It was a joint undertaking by the British Admiralty, Admiralty and the Secretary of ... [...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 t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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