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Thomson Head
Thomson Head () is a steep, rocky headland rising to 915 m at the east side of Bourgeois Fjord, between Perutz and Bader Glaciers, forming the north extremity of German Peninsula on Fallières Coast on the west side of Graham Land, Antarctica. First surveyed in 1936 by the British Graham Land Expedition (BGLE) under Rymill. Resurveyed in 1948-49 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 ... (FIDS) and named for William H. Thomson, FIDS air pilot at Stonington Island in 1947. Map * British Antarctic Territory. Scale 1:200000 topographic map. DOS 610 Series, Sheet W 67 66. Directorate of Overseas Surveys, Tolworth, UK, 1978. References SCAR Composite Antarctic Gazetteer Headlands of Graham Land Fallières Coast {{Fall ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Headland
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bourgeois Fjord
Bourgeois Fjord is an inlet, long in a northeast–southwest direction and wide, lying between the east sides of Pourquoi Pas Island and Blaiklock Island and the west coast of Graham Land. It separates Loubet Coast to the north from Fallières Coast to the south. The fjord was discovered by the French Antarctic Expedition, 1908–10, under Jean-Baptiste Charcot, and named by him for Colonel Joseph E. Bourgeois, Director of the Geographic Service of the French Army. The outline of this inlet was more accurately delineated in 1936 by the British Graham Land Expedition under John Rymill. Map * British Antarctic Territory. Scale 1:200000 topographic map. DOS 610 Series, Sheet W 67 66. Directorate of Overseas Surveys, Tolworth, UK, 1978. See also * Lliboutry Glacier Lliboutry Glacier () is a glacier flowing southwest from the Boyle Mountains of Antarctica into Bourgeois Fjord, Loubet Coast. It was named by the UK Antarctic Place-Names Committee in 1983 after Louis A.F. Lliboutry, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Perutz Glacier
Perutz Glacier () is a glacier, 10 nautical miles (18 km) long and 2 nautical miles (3.7 km) wide, which flows west-northwest from Hemimont Plateau into Bourgeois Fjord, close east of Thomson Head, on the west coast of Graham Land, Antarctica. The mouth of the glacier was first surveyed in 1936 by the British Graham Land Expedition (BGLE) under Rymill. The entire glacier was surveyed in 1946-47 and 1948-49 by the Falkland Islands Dependencies Survey (FIDS), and named by them for Max F. Perutz of the Cavendish Laboratory The Cavendish Laboratory is the Department of Physics at the University of Cambridge, and is part of the School of Physical Sciences. The laboratory was opened in 1874 on the New Museums Site as a laboratory for experimental physics and is named ..., Cambridge, who has made important studies on the mechanism of glacier flow. Glaciers of Fallières Coast {{FallièresCoast-glacier-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bader Glacier
Bader Glacier () is a small glacier draining the west slopes of Rudozem Heights and flowing to Bourgeois Fjord just south of Thomson Head on German Peninsula, Fallières Coast on the west side of Graham Land, Antarctica. History It was named by the UK Antarctic Place-Names Committee in 1958 for Swiss glaciologist Henri Bader of Rutgers University (U.S.), author of an important thesis on the development of the snowflake and its metamorphoses. See also * List of glaciers in the Antarctic * Glaciology Map * British Antarctic Territory. Scale 1:200000 topographic map. DOS 610 Series, Sheet W 67 66. Directorate of Overseas Surveys, Tolworth, UK, 1978. References * Glaciers of Fallières Coast {{FallièresCoast-glacier-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
German Peninsula
German Peninsula ( bg, полуостров Герман, translit=Poluostrov German) is the mountainous peninsula projecting from the north end of Fallières Coast in Graham Land, Antarctica 11.4 km in west direction between Bourgeois Fjord to the north and west, and Dogs Leg Fjord to the south. It is extending 15.9 km between Thomson Head to the north and Bottrill Head to the southwest, with its interior occupied by Rudozem Heights. The peninsula is named after the settlement of German in Western Bulgaria, now part of the city of Sofia. Location German Peninsula is centred at . British mapping in 1978. Maps * British Antarctic Territory. Scale 1:200000 topographic map. DOS 610 Series, Sheet W 67 66. Directorate of Overseas Surveys, Tolworth, UK, 1978. Antarctic Digital Database (ADD).Scale 1:250000 topographic map of Antarctica. Scientific Committee on Antarctic Research (SCAR), 1993–2016. References German Peninsula.SCAR Composite Antarctic Gazetteer. Bulgarian Anta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fallières Coast
The Fallières Coast is that portion of the west coast of the Antarctic Peninsula between the head of Bourgeois Fjord and Cape Jeremy and lies on Marguerite Bay and the Wordie Ice Shelf. On the south it is joined by Rymill Coast, and in the north by Loubet Coast. Fallières Coast was first explored in January 1909 by the French Antarctic Expedition under J.B. Charcot, who named it for Armand Fallières, then President of France The president of France, officially the president of the French Republic (french: Président de la République française), is the executive head of state of France, and the commander-in-chief of the French Armed Forces. As the presidency is .... References Coasts of Graham Land {{FallièresCoast-geo-stub ... [...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] |
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 ve ... [...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] |
William H
William is a masculine given name of Norman French origin.Hanks, Hardcastle and Hodges, ''Oxford Dictionary of First Names'', Oxford University Press, 2nd edition, , p. 276. It became very popular in the English language after the Norman conquest of England in 1066,All Things William"Meaning & Origin of the Name"/ref> and remained so throughout the Middle Ages and into the modern era. It is sometimes abbreviated "Wm." Shortened familiar versions in English include Will, Wills, Willy, Willie, Liam, Bill, and Billy. A common Irish form is Liam. Scottish diminutives include Wull, Willie or Wullie (as in Oor Wullie or the play ''Douglas''). Female forms are Willa, Willemina, Wilma and Wilhelmina. Etymology William is related to the German given name ''Wilhelm''. Both ultimately descend from Proto-Germanic ''*Wiljahelmaz'', with a direct cognate also in the Old Norse name ''Vilhjalmr'' and a West Germanic borrowing into Medieval Latin ''Willelmus''. The Proto-Germa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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