Tasman Ridge
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Tasman Ridge
Tasman Ridge () is a ridge, 3 nautical miles (6 km) long, located 10 nautical miles (18 km) northeast of Mount Hooker, bounded on the northwest by Ball Glacier and on the southeast by Hooker Glacier, descending into Blue Glacier in the Royal Society Range, Victoria Land. Named by New Zealand Geographic Board (NZGB) in 1994 in association with other names from Mount Cook National Park Mount Cook National Park may refer to the following: *Mount Cook National Park, Australia *Aoraki / Mount Cook National Park Aoraki/Mount Cook National Park is in the South Island of New Zealand. Aoraki / Mount Cook, New Zealand's highest mo ... that are found in this area. Ridges of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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Mount Hooker (Antarctica)
Mount Hooker () is a rounded summit over high, standing immediately south of Mount Lister in the Royal Society Range of Victoria Land, Antarctica. It was discovered by the British National Antarctic Expedition, 1901–04, which named it for Sir Joseph Dalton Hooker Sir Joseph Dalton Hooker (30 June 1817 – 10 December 1911) was a British botanist and explorer in the 19th century. He was a founder of geographical botany and Charles Darwin's closest friend. For twenty years he served as director of t .... References Royal Society Range Mountains of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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Ball Glacier (Victoria Land)
Ball Glacier is a glacier long with the head located between Mount Lister and Mount Hooker on the east side of the Royal Society Range. The glacier flows northeast between Craw Ridge and Tasman Ridge into Blue Glacier. It was named by the New Zealand Geographic Board after Gary Ball, a New Zealand mountaineer who climbed Mount Lister with an Italian field party, 1976–77, and camped on this glacier; he was field assistant with R.H. Findlay's New Zealand Antarctic Research Program party to this area, 1980–81. See also * List of glaciers in the Antarctic * Glaciology Glaciology (; ) is the scientific study of glaciers, or more generally ice and natural phenomena that involve ice. Glaciology is an interdisciplinary Earth science that integrates geophysics, geology, physical geography, geomorphology, c ... * Ball Peak References Glaciers of Scott Coast {{ScottCoast-glacier-stub ...
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Hooker Glacier (Antarctica)
Hooker Glacier () is a glacier on the east side of the Royal Society Range, draining northeast into Blue Glacier from the slopes of Mount Hooker. It was surveyed in 1957 by the New Zealand Blue Glacier Party of 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) and named after Mount Hooker. Glaciers of Victoria Land {{VictoriaLand-glacier-stub ...
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Blue Glacier (Antarctica)
Blue Glacier is a large glacier which flows into Bowers Piedmont Glacier about south of New Harbour, in Victoria Land, Antarctica. Robbins Hill is the East-most rock unit on the north side of the terminus of the glacier. It was discovered by the British National Antarctic Expedition under Robert Falcon Scott Captain Robert Falcon Scott, , (6 June 1868 – c. 29 March 1912) was a British Royal Navy officer and explorer who led two expeditions to the Antarctic regions: the ''Discovery'' expedition of 1901–1904 and the ill-fated ''Terra Nov ..., 1901–04, who gave it this name because of its clear blue ice at the time of discovery. References * Glaciers of Scott Coast {{ScottCoast-glacier-stub ...
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Royal Society Range
The Royal Society Range () is a mountain range in Victoria Land, Antarctica. With its summit at , the massive Mount Lister forms the highest point in this range. Mount Lister is located along the western shore of McMurdo Sound between the Koettlitz, Skelton and Ferrar glaciers. Other notable local terrain features include Allison Glacier, which descends from the west slopes of the Royal Society Range into Skelton Glacier. Discovery and naming The range was probably first seen by Captain James Clark Ross in 1841. The range was explored by the British National Antarctic Expedition (BrNAE) under Robert Falcon Scott, who named the range after the Royal Society and applied names of its members to many of its peaks. For example, Mount Lister was named for Lord Joseph Lister, President of the Royal Society, 1895–1900. The Royal Society provided financial support to the expedition and its members had assisted on the committee which organized the expedition. Geology The Royal S ...
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Victoria Land
Victoria Land is a region in eastern Antarctica which fronts the western side of the Ross Sea and the Ross Ice Shelf, extending southward from about 70°30'S to 78°00'S, and westward from the Ross Sea to the edge of the Antarctic Plateau. It was discovered by Captain James Clark Ross in January 1841 and named after Queen Victoria. The rocky promontory of Minna Bluff is often regarded as the southernmost point of Victoria Land, and separates the Scott Coast to the north from the Hillary Coast of the Ross Dependency to the south. The region includes ranges of the Transantarctic Mountains and the McMurdo Dry Valleys (the highest point being Mount Abbott in the Northern Foothills), and the flatlands known as the Labyrinth. The Mount Melbourne is an active volcano in Victoria Land. Early explorers of Victoria Land include James Clark Ross and Douglas Mawson. In 1979, scientists discovered a group of 309 meteorites in Antarctica, some of which were found near the Allan Hills in ...
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New Zealand Geographic Board
The New Zealand Geographic Board Ngā Pou Taunaha o Aotearoa (NZGB) was established by the New Zealand Geographic Board Act 1946, which has since been replaced by the New Zealand Geographic Board (Ngā Pou Taunaha o Aotearoa) Act 2008. Although an independent institution, it is responsible to the Minister for Land Information. The board has authority over geographical and hydrographic names within New Zealand and its territorial waters. This includes the naming of small urban settlements, localities, mountains, lakes, rivers, waterfalls, harbours and natural features and may include researching local Māori names. It has named many geographical features in the Ross Sea region of Antarctica. It has no authority to alter street names (a local body responsibility) or the name of any country. The NZGB secretariat is part of Toitū Te Whenua Land Information New Zealand (LINZ) and provides the board with administrative and research assistance and advice. The New Zealand Geograph ...
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Aoraki/Mount Cook National Park
Aoraki/Mount Cook National Park is in the South Island of New Zealand. Aoraki / Mount Cook, New Zealand's highest mountain, and the eponymous village lie within the park. The area was gazetted as a national park in October 1953 and consists of reserves that were established as early as 1887 to protect the area's significant vegetation and landscape. Even though most of the park is alpine terrain, it is easily accessible. The only road access into Aoraki/Mount Cook National Park is via , which starts near Twizel, at distance the closest town to the park, and leads directly to Mount Cook Village, where the road ends. The village is situated within the park, however, it consists only of a hotel and motels, as well as housing and amenities for the staff of the hotel and motels and other support personnel. Geography The park stretches for about along the southwest–northeast direction of the Southern Alps, covering on the southeastern side of the main spine of the Alps. The ...
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Ridges Of Victoria Land
A ridge or a mountain ridge is a geographical feature consisting of a chain of mountains or hills that form a continuous elevated crest for an extended distance. The sides of the ridge slope away from the narrow top on either side. The lines along the crest formed by the highest points, with the terrain dropping down on either side, are called the ridgelines. Ridges are usually termed hills or mountains as well, depending on size. Smaller ridges, especially those leaving a larger ridge, are often referred to as spurs. Types There are several main types of ridges: ;Dendritic ridge: In typical dissected plateau terrain, the stream drainage valleys will leave intervening ridges. These are by far the most common ridges. These ridges usually represent slightly more erosion resistant rock, but not always – they often remain because there were more joints where the valleys formed or other chance occurrences. This type of ridge is generally somewhat random in orientation, often ...
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