|
Longstaff Peaks
The Longstaff Peaks () are a series of high peaks standing just west of Davidson Glacier in the north-central part of the Holland Range in Antarctica. They were discovered by the British National Antarctic Expedition (1901–04), and named ''Mount Longstaff'' for Llewellyn Wood Longstaff, a principal contributor to the expedition. The descriptive term was amended by the New Zealand Antarctic Place-Names Committee New Zealand Antarctic Place-Names Committee (NZ-APC) is an adjudicating committee established to authorize the naming of features in the Ross Dependency on the Antarctic continent. It is composed of the members of the New Zealand Geographic Board p .... References Mountains of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Davidson Glacier (Antarctica)
The Holland Range () is a rugged coastal mountain range in Antarctica, about long, lying just west of the Ross Ice Shelf and extending from Robb Glacier to Lennox-King Glacier. It was named by the Ross Sea Committee for Sir Sidney Holland, who as Prime Minister of New Zealand supported that nation's participation in the Commonwealth Trans-Antarctic Expedition The Commonwealth Trans-Antarctic Expedition (CTAE) of 1955–1958 was a Commonwealth-sponsored expedition that successfully completed the first overland crossing of Antarctica, via the South Pole. It was the first expedition to reach the South ... (1956–58). References Mountain ranges of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Holland Range
The Holland Range () is a rugged coastal mountain range in Antarctica, about long, lying just west of the Ross Ice Shelf and extending from Robb Glacier to Lennox-King Glacier. It was named by the Ross Sea Committee for Sir Sidney Holland, who as Prime Minister of New Zealand supported that nation's participation in the Commonwealth Trans-Antarctic Expedition The Commonwealth Trans-Antarctic Expedition (CTAE) of 1955–1958 was a Commonwealth-sponsored expedition that successfully completed the first overland crossing of Antarctica, via the South Pole. It was the first expedition to reach the South ... (1956–58). References Mountain ranges of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
British National Antarctic Expedition
The ''Discovery'' Expedition of 1901–1904, known officially as the British National Antarctic Expedition, was the first official British exploration of the Antarctic regions since the voyage of James Clark Ross sixty years earlier (1839–1843). Organized on a large scale under a joint committee of the Royal Society and the Royal Geographical Society (RGS), the new expedition carried out scientific research and geographical exploration in what was then largely an untouched continent. It launched the Antarctic careers of many who would become leading figures in the Heroic Age of Antarctic Exploration, including Robert Falcon Scott who led the expedition, Ernest Shackleton, Edward Wilson, Frank Wild, Tom Crean and William Lashly. Its scientific results covered extensive ground in biology, zoology, geology, meteorology and magnetism. The expedition discovered the existence of the only snow-free Antarctic valleys, which contains the longest river of Antarctica. Further ach ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Llewellyn Wood Longstaff
Lieutenant-Colonel Llewellyn Wood Longstaff (23 December 1841 – 20 November 1918) was an English industrialist and fellow of the Royal Geographical Society. He is best known for being the chief private-sector patron and financial angel of the Discovery Expedition to the Antarctic. Antarctic patron Llewellyn Longstaff was born in Wandsworth London, on 23 December 1841. In 1873, he married Marie Lydia Sawyer, with whom he had 10 children, including mountaineer Tom George Longstaff. He owned a significant equity share in Blundell Spence & Co., a £400,000 firm based in Kingston upon Hull that crushed linseed oil to manufacture oil paint. He was also a member of several nongovernmental organizations, including the Freemasons, the Hull Chamber of Commerce and Shipping, and the Royal Geographical Society (RGS). Longstaff's Society membership coincided with the presidency of longtime RGS leader Sir Clements Markham, whose dream was to organize a British expedition to the then-unkno ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand Antarctic Place-Names Committee
New Zealand Antarctic Place-Names Committee (NZ-APC) is an adjudicating committee established to authorize the naming of features in the Ross Dependency on the Antarctic continent. It is composed of the members of the New Zealand Geographic Board plus selected specialists on Antarctica. This committee works in collaboration with similar place-naming authorities in Australia, Great Britain and the United States to reach concurrence on each decision. The NZ-APC committee was established in 1956. Names attributed by the committee * Alberich Glacier, named after Alberich, king of the elves and chief of the Nibelungen * Arena Saddle, named in conjunction with Arena Valley * Brawhm Pass, named after the six party members of the University of New South Wales expeditions of 1964–65 and 1966–67 * Caliper Cove, named for descriptive features * Canada Stream, named in conjunction with Canada Glacier * Cape Crossfire, named for descriptive features * Cuneiform Cliffs, named for des ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of The Ross Dependency
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] |
