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Ārai Terraces
The Ārai Terraces () are a series of crevassed terraces and icefalls close southward of Fazekas Hills, near the head of Lowery Glacier. Name The Ārai Terraces were so named by the New Zealand Geological Survey Antarctic Expedition (NZGSAE; 1959–60) because they are a natural barrier to sledge travel which the party was unable to traverse, ''ārai'' being the Māori term for barrier. Location The Ārai Terraces are in the eastern Queen Elizabeth Range to the northeast of the Prince Andrew Plateau, east of the Moore Mountains and Mount Rabot. The Linehan Glacier and Lowery Glacier define the western boundary, and the Robb Glacier the eastern boundary. Features around the Ārai Terraces include Bengaard Peak to the south, Softbed Ridges, Fazekas Hills and Mount Oona to the north. Features Bengaard Peak . Prominent rock peak, high, located south of Fazekas Hills, on the east side of Queen Elizabeth Range. Named by the United States Advisory Committee on Antarctic Names ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Queen Elizabeth Range (Antarctica)
The Queen Elizabeth Range is a rugged mountain range of the Transantarctic Mountains System, located in the Ross Dependency region of Antarctica. It parallels the eastern side of Marsh Glacier for nearly from Nimrod Glacier in the north to Law Glacier in the south. Mount Markham (4,350 m), is the highest elevation in the range. Named by J.H. Miller of the New Zealand party of the Commonwealth Trans-Antarctic Expedition (1956–58) who, with G.W. Marsh, explored this area. It was named for Queen Elizabeth II, the patron of the expedition. Geological features Mount Bonaparte Mount Bonaparte () is a mountain, high, standing 4 mi NW of Mount Lecointe. Discovered by the British Antarctic Expedition (1907–09) under Shackleton, and named for Prince Roland Bonaparte, President of the Société de Géographie of Paris from 1910-1924. Inaccessible Cliffs Inaccessible Cliffs () is a line of steep cliffs, interrupted by several glaciers, which form the northern escarpment o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lowery Glacier
Lowery Glacier () is a glacier about long, which flows north from Prince Andrew Plateau, Antarctica, along the east side of the Queen Elizabeth Range to enter Nimrod Glacier. It was named by the New Zealand Geological and Topographical Survey Expedition (1959–60) for J.H. Lowery who, as a member of a field party, suffered injuries when a Sno-cat broke through a crevasse bridge off Cape Selborne Cape Selborne () is a high snow-covered cape at the south side of Barne Inlet, the terminus of Byrd Glacier at the west side of the Ross Ice Shelf. Discovered by the ''Discovery'' expedition (1901–1904) and named for William Waldegrave Palmer Se ... in November 1959. References Glaciers of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand Geological Survey Antarctic Expedition
The New Zealand Geological Survey Antarctic Expedition (NZGSAE) describes a series of scientific explorations of the continent Antarctica. The expeditions were notably active throughout the 1950s and 1960s. Features named by the expeditions 1957–1958 expedition The 1957–1958 expedition went to the Ross Dependency and named the Borchgrevink Glacier. Other features named include: * Carter Ridge * Felsite Island * Halfway Nunatak * Hedgehog Island * Moraine Ridge 1958–1959 expedition * Cadwalader Beach * Cape Hodgson * Carter Ridge * Isolation Point * Mountaineer Range * Mount Aurora * Mount Hayward * Mount Henderson (White Island) * Mount Bird. 1960–1961 expedition * Deverall Island * Lonewolf Nunataks 1961–1962 expedition * Aurora Heights * The Boil * Ford Spur * Graphite Peak * Half Century Nunatak * Half Dome Nunatak * Hump Passage * Last Cache Nunatak * Lookout Dome * Montgomerie Glacier * Mount Fyfe * Mount Macdonald * Snowshoe Pass * Turret Nu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Māori Language
Māori (), or ('the Māori language'), also known as ('the language'), is an Eastern Polynesian language spoken by the Māori people, the indigenous population of mainland New Zealand. Closely related to Cook Islands Māori, Tuamotuan, and Tahitian, it gained recognition as one of New Zealand's official languages in 1987. The number of speakers of the language has declined sharply since 1945, but a Māori-language revitalisation effort has slowed the decline. The 2018 New Zealand census reported that about 186,000 people, or 4.0% of the New Zealand population, could hold a conversation in Māori about everyday things. , 55% of Māori adults reported some knowledge of the language; of these, 64% use Māori at home and around 50,000 people can speak the language "very well" or "well". The Māori language did not have an indigenous writing system. Missionaries arriving from about 1814, such as Thomas Kendall, learned to speak Māori, and introduced the Latin alphabet. In 1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prince Andrew Plateau
Prince Andrew Plateau () is an ice-covered plateau, about long and wide, lying south of Mount Rabot in the Queen Elizabeth Range of Antarctica. Exploration and name The Prince Andrew Plateau was named by the New Zealand Geological Survey Antarctic Expedition (NZGSAE) (1961-62) for Prince Andrew, son of Queen Elizabeth II of Great Britain. Location The Prince Andrew Plateau is in the southern Queen Elizabeth Range between the Moore Mountains and Ārai Terraces to the north and the Peletier Plateau to the south. The Marsh Glacier is to the west and the Bowden Névé to the east. Features to the east include Painted Cliffs in the southeast, which include Dawson Peak and Mount Picciotto and the Disch Promontary further north. Features to the west include Dakota Pass in the south, Cranfield Peak, Mount Weeks and New Year Pass to the south of the Moore Mountains. Features to the north include Helm Glacier, Linehan Glacier, Turnabout Ridge, January Col, Claydon Peak and Baulch Pea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moore Mountains
The Moore Mountains () are a small but conspicuous group of mountains just north of New Year Pass in the Queen Elizabeth Range in Antarctica. They were observed in 1957 by the New Zealand southern 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 for R.D. Moore, Treasurer of the Ross Sea Committee. References Mountain ranges of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Rabot
Mount Rabot () is a mountain, high, standing southeast of Mount Lecointe in the Queen Elizabeth Range in Antarctica. Name Mount Rabot was discovered and named by the British Antarctic Expedition (BrAE; 1907-09). Charles Rabot was editor of ''La Géographie'', bulletin of the Société Geographique, Paris, and was an outstanding glaciologist of that period. Location Mount Rabot is in the center of the Queen Elizabeth Range, to the east of the Marsh Glacier and west of the Helm Glacier. The Moore Mountains and Prince Andrew Plateau are to the south. Markham Plateau is to the north. Features near Mount Rabot include Solitary Peak to the south, Mount Counts and Rabot Glacier to the west, Moody Nunatak, Bartrum Plateau and Mount Bonaparte to the northwest, Mount Lecointe to the north, Fopay Peak and Mount Macbain to the northeast. Features Solitary Peak . A peak high located southeast of Mount Rabot. An important geologic section was measured on the feature by the Ohio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Linehan Glacier
Lowery Glacier () is a glacier about long, which flows north from Prince Andrew Plateau, Antarctica, along the east side of the Queen Elizabeth Range to enter Nimrod Glacier. It was named by the New Zealand Geological and Topographical Survey Expedition (1959–60) for J.H. Lowery who, as a member of a field party, suffered injuries when a Sno-cat broke through a crevasse A crevasse is a deep crack, that forms in a glacier or ice sheet that can be a few inches across to over 40 feet. Crevasses form as a result of the movement and resulting stress associated with the shear stress generated when two semi-rigid pie ... bridge off Cape Selborne in November 1959. References Glaciers of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Robb Glacier
Robb Glacier () is a glacier about 40 nautical miles (70 km) long, flowing from Clarkson Peak north along the east side of Softbed Ridges to the Ross Ice Shelf at Cape Goldie. Named by the expedition after Murray Robb, leader of the New Zealand Geological Survey Antarctic Expedition The New Zealand Geological Survey Antarctic Expedition (NZGSAE) describes a series of scientific explorations of the continent Antarctica. The expeditions were notably active throughout the 1950s and 1960s. Features named by the expeditions 1957 ... (NZGSAE) (1959–60), who traversed this glacier to reach Lowery Glacier. See also * Cape Huinga * Whakawhiti Saddle * Worthley Peak References Glaciers of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Advisory Committee On Antarctic Names
The Advisory Committee on Antarctic Names (ACAN or US-ACAN) is an advisory committee of the United States Board on Geographic Names responsible for recommending commemorative names for features in Antarctica. History The committee was established in 1943 as the Special Committee on Antarctic Names (SCAN). It became the Advisory Committee on Antarctic Names in 1947. Fred G. Alberts was Secretary of the Committee from 1949 to 1980. By 1959, a structured nomenclature was reached, allowing for further exploration, structured mapping of the region and a unique naming system. A 1990 ACAN gazeeter of Antarctica listed 16,000 names. Description The United States does not recognise territorial boundaries within Antarctica, so ACAN assigns names to features anywhere within the continent, in consultation with other national nomenclature bodies where appropriate, as defined by the Antarctic Treaty System. The research and staff support for the ACAN is provided by the United States Geologi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crevasse Fields Of The Ross Dependency
A crevasse is a deep crack, that forms in a glacier or ice sheet that can be a few inches across to over 40 feet. Crevasses form as a result of the movement and resulting stress associated with the shear stress generated when two semi-rigid pieces above a plastic substrate have different rates of movement. The resulting intensity of the shear stress causes a breakage along the faces. Description Crevasses often have vertical or near-vertical walls, which can then melt and create seracs, arches, and other ice formations. These walls sometimes expose layers that represent the glacier's stratigraphy. Crevasse size often depends upon the amount of liquid water present in the glacier. A crevasse may be as deep as 45 metres and as wide as 20 metres. by |
