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Nodwell Peaks
Nodwell Peaks () are two outstanding peaks, less than 1 mile apart, on the east side of Edgeworth Glacier, Graham Land. It is situated 3 km north-northwest of Skidoo Nunatak and 5.2 km west of Maslarov Nunatak. Mapped from surveys by Falkland Islands Dependencies Survey (FIDS) (1960–61). Named by United Kingdom Antarctic Place-Names Committee (UK-APC) after Robin-Nodwell Mfg. Ltd. of Calgary, Canada, makers of Nodwell tracked carriers which were invented by Bruce Nodwell Bruce Nodwell, (May 12, 1914 – January 20, 2006) was a Canadian inventor who invented the ''Nodwell 110'', a multi-purpose two-tracked vehicle capable of traversing a wide variety of adverse terrain, including sand, mud, muskeg, swamp, and ..., and used in Antarctica since 1960. Mountains of Graham Land Nordenskjöld Coast {{NordenskjöldCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Edgeworth Glacier
The Edgeworth Glacier () is a glacier long, flowing south-southwestwards from the edge of Detroit Plateau below Wolseley Buttress to the ice shelf west of Sobral Peninsula, Graham Land, Antarctica. Location Edgeworth Glacier is in Graham Land on the Nordenskjöld Coast of the eastern Antarctic Peninsula. It flows south from the Detroit Plateau, past the Sobral Peninsula to the east to enter the Weddell Sea. Copernix satellite view Mapping and name The Edgeworth Glacier was mapped from surveys by the Falkland Islands Dependencies Survey (FIDS) in 1960–61, and was named by the UK Antarctic Place-Names Committee (UK-APC) for Richard Lovell Edgeworth, the British inventor of the "portable railway," the first Continuous track, track-laying vehicle, in 1770. Features Bombardier Glacier . A glacier flowing southeast from the edge of Detroit Plateau, and through a deep trough to join Edgeworth Glacier. Mapped from surveys by FIDS (1960-61). Named by UK-APC for Joseph-Armand Bomb ... [...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] |
Skidoo Nunatak
The Sobral Peninsula () is a high and mainly ice-covered peninsula in northern Graham Land, Antarctica. The feature is long and wide and projects southward into the northern part of the Larsen Ice Shelf west of Larsen Inlet. Location The Sobral Peninsula lies towards the east end of the Nordenskjöld Coast of the Antarctic Peninsula. It extends southward into the Weddell Sea. The Detroit Plateau and Mount Hornsby are to the north. To the east, Larsen Inlet separates the Sobral Peninsula from Mount Tucker and the Longing Peninsula. The Edgeworth Glacier flows into Mundraga Bay to the west. Copernix satellite image Name The name "Sobral Peninsula" was applied by UK Antarctic Place-Names Committee (UK-APC) in 1963, and derives from Cape Sobral at the south end of this peninsula. Features Features and nearby features, from north to south, include: Ferguson Ridge . A ridge trending north-northwest – south-southeast and rising to high southwest of Nodwell Peaks. Named in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maslarov Nunatak
Maslarov Nunatak ( bg, Масларов нунатак, Maslarov nunatak, ) is the rocky ridge 1.9 km long in northwest–southeast direction and 1.3 km wide, rising to 697 mReference Elevation Model of Antarctica. Polar Geospatial Center. University of Minnesota, 2019 at the northwest coast of on in , |
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 Admiralty and the Colonial Office. At the end of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bruce Nodwell
Bruce Nodwell, (May 12, 1914 – January 20, 2006) was a Canadian inventor who invented the ''Nodwell 110'', a multi-purpose two-tracked vehicle capable of traversing a wide variety of adverse terrain, including sand, mud, muskeg, swamp, and snow. In 1970, he was made an Officer of the Order of Canada, Canada's highest civilian honor, "for his contribution to the opening of the Canadian North through his inventions and development of various types of tracked vehicles". A mountain in Antarctica " Nodwell Peaks" and a lake in NWT bear his name. Early life William Bruce Nodwell was born on his father's homestead near Asquith, Saskatchewan, May 12, 1914. His unusual birth certificate read ''Section 22, Township 36, Range 9 west 3rd.'' As a youngster, his family lived in many small western Canadian towns, as his father was a grain elevator operator and trainer. They returned to Asquith, where his father ran a hardware store and later a Dodge car dealership in North Battleford. Du ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Graham Land
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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