|
Lanterman Range
The Lanterman Range () is a mountain range about long and wide, forming the southwest part of the Bowers Mountains in Antarctica. It is bounded by the Rennick Glacier, Sledgers Glacier, Black Glacier and Canham Glacier. Exploration and naming The range was mapped by United States Geological Survey (USGS) from surveys and United States Navy air photos, 1960–62. It was named by the United States Advisory Committee on Antarctic Names (US-ACAN) for Commander William Lanterman, an aerological officer for U.S. Navy Operation Deep Freeze, 1959–62. Location The Lanterman Range lies to the east of the Rennick Glacier and its tributary Canham Glacier. The Sledgers Glacier flows past its northeast end. The MacKinnon Glacier drains the range to the north into Sledgers Glacier. Glaciers draining to the west include Orr Glacier, Linder Glacier, Hunter Glacier, Hoshko Glacier, Zenith Glacier and Johnstone Glacier. The Molar Massif lies to the east. The Crown Hills form the sout ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Orr Glacier
Rennick Glacier is broad glacier, nearly long, which is one of the largest in Antarctica. It rises on the polar plateau westward of Mesa Range and is wide, narrowing to near the coast. It takes its name from Rennick Bay where the glacier reaches the sea. The seaward part of the glacier was photographed by U.S. Navy (USN) Operation Highjump, 1946–47. The upper reaches of the Rennick Glacier were discovered and explored by the U.S. Victoria Land Traverse (VLT) in February 1960, and the first ascent made of Welcome Mountain by John Weihaupt, Alfred Stuart, Claude Lorius and Arnold Heine of the VLT party. On February 10, 1960, Lieutenant Commander Robert L. Dale, pilot of U.S. Navy (USN) Squadron VX-6, evacuated the VLT from 7238S, 16132E, on this glacier, and then conducted an aerial photographic reconnaissance to Rennick Bay on the coast before returning the VLT team to McMurdo Station. Features * Illusion Hills, small hills on the glacier * Litell Rocks, an area of rock outcr ... [...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] |
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] |
Crown Hills (Antarctica)
The Crown Hills () are a group of peaks and hills forming the south-east part of the Lanterman Range in the Bowers Mountains of Victoria Land, Antarctica. Lying between Zenith Glacier and Gambone Peak, and including All Black Peak, they rise to a height of . The name was given by the New Zealand Antarctic Place-Names Committee (NZ-APC) in 1983, at the suggestion of geologist M.G. Laird, in association with nearby Coronet Peak. Location The Crown Hills are at the southeast end of the Lanterman Range. The Canham Glacier flows northwest along their southwest margin, and the Black Glacier flows northeast along their southeast margin. They are drained to the south by the Zenith Glacier and the Johnstone Glacier. The Molar Massif is to the north, the Alamein Range to the southwest and the Salamander Range to the south. The Leitch Massif and King Range are to the east. Features Half Black Peak . A peak ME of Mount Edixon, rising to over high in the southeast part of Lanter ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Molar Massif
Molar Massif () is a large mountain massif immediately east of the Lanterman Range in the Bowers Mountains of Antarctica. It was mapped by the United States Geological Survey from ground surveys and U.S. Navy air photos, 1960–1964. The descriptive name was applied by the Advisory Committee on Antarctic Names; when viewed in plan, the outline of the massif resembles a molar tooth. Features Geographical features include: * Canine Hills * Dentine Peak * Evison Glacier * Husky Pass * Incisor Ridge * Leap Year Glacier * Tobogganers Icefall * Wisdom Hills Further reading * Gunter Faure, Teresa M. Mensing, The Transantarctic Mountains: Rocks, Ice, Meteorites and Water', P 136 * Edmund Stump, The Ross Orogen of the Transantarctic Mountains', P 49 External links Molar Massifon USGS website Molar Massifon AADC website Molar Massifon SCAR A scar (or scar tissue) is an area of fibrous tissue that replaces normal skin after an injury. Scars result from the biological ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Johnstone Glacier
The Crown Hills () are a group of peaks and hills forming the south-east part of the Lanterman Range in the Bowers Mountains of Victoria Land, Antarctica. Lying between Zenith Glacier and Gambone Peak, and including All Black Peak, they rise to a height of . The name was given by the New Zealand Antarctic Place-Names Committee (NZ-APC) in 1983, at the suggestion of geologist M.G. Laird, in association with nearby Coronet Peak. Location The Crown Hills are at the southeast end of the Lanterman Range. The Canham Glacier flows northwest along their southwest margin, and the Black Glacier flows northeast along their southeast margin. They are drained to the south by the Zenith Glacier and the Johnstone Glacier. The Molar Massif is to the north, the Alamein Range to the southwest and the Salamander Range to the south. The Leitch Massif and King Range are to the east. Features Half Black Peak . A peak ME of Mount Edixon, rising to over high in the southeast part of Lanter ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zenith Glacier
The Crown Hills () are a group of peaks and hills forming the south-east part of the Lanterman Range in the Bowers Mountains of Victoria Land, Antarctica. Lying between Zenith Glacier and Gambone Peak, and including All Black Peak, they rise to a height of . The name was given by the New Zealand Antarctic Place-Names Committee (NZ-APC) in 1983, at the suggestion of geologist M.G. Laird, in association with nearby Coronet Peak. Location The Crown Hills are at the southeast end of the Lanterman Range. The Canham Glacier flows northwest along their southwest margin, and the Black Glacier flows northeast along their southeast margin. They are drained to the south by the Zenith Glacier and the Johnstone Glacier. The Molar Massif is to the north, the Alamein Range to the southwest and the Salamander Range to the south. The Leitch Massif and King Range are to the east. Features Half Black Peak . A peak ME of Mount Edixon, rising to over high in the southeast part of Lanter ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hoshko Glacier
The Crown Hills () are a group of peaks and hills forming the south-east part of the Lanterman Range in the Bowers Mountains of Victoria Land, Antarctica. Lying between Zenith Glacier and Gambone Peak, and including All Black Peak, they rise to a height of . The name was given by the New Zealand Antarctic Place-Names Committee (NZ-APC) in 1983, at the suggestion of geologist M.G. Laird, in association with nearby Coronet Peak. Location The Crown Hills are at the southeast end of the Lanterman Range. The Canham Glacier flows northwest along their southwest margin, and the Black Glacier flows northeast along their southeast margin. They are drained to the south by the Zenith Glacier and the Johnstone Glacier. The Molar Massif is to the north, the Alamein Range to the southwest and the Salamander Range to the south. The Leitch Massif and King Range are to the east. Features Half Black Peak . A peak ME of Mount Edixon, rising to over high in the southeast part of Lanter ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hunter Glacier
Rennick Glacier is broad glacier, nearly long, which is one of the largest in Antarctica. It rises on the polar plateau westward of Mesa Range and is wide, narrowing to near the coast. It takes its name from Rennick Bay where the glacier reaches the sea. The seaward part of the glacier was photographed by U.S. Navy (USN) Operation Highjump, 1946–47. The upper reaches of the Rennick Glacier were discovered and explored by the U.S. Victoria Land Traverse (VLT) in February 1960, and the first ascent made of Welcome Mountain by John Weihaupt, Alfred Stuart, Claude Lorius and Arnold Heine of the VLT party. On February 10, 1960, Lieutenant Commander Robert L. Dale, pilot of U.S. Navy (USN) Squadron VX-6, evacuated the VLT from 7238S, 16132E, on this glacier, and then conducted an aerial photographic reconnaissance to Rennick Bay on the coast before returning the VLT team to McMurdo Station. Features * Illusion Hills, small hills on the glacier * Litell Rocks, an area of rock outcr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Linder Glacier
Linder Glacier () is a steep tributary glacier in the Lanterman Range, Bowers Mountains, Antarctica. It drains the southern slopes of Mount Bernstein and moves south to enter Hunter Glacier. The glacier was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–62, and was named by the Advisory Committee on Antarctic Names for Lieutenant Michael A. Linder, U.S. Navy Reserve, a communications and administrative officer with the McMurdo Station McMurdo Station is a United States Antarctic research station on the south tip of Ross Island, which is in the New Zealand-claimed Ross Dependency on the shore of McMurdo Sound in Antarctica. It is operated by the United States through the Unit ... winter party, 1967. References Glaciers of Pennell Coast {{PennellCoast-glacier-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
MacKinnon Glacier
Rennick Glacier is broad glacier, nearly long, which is one of the largest in Antarctica. It rises on the polar plateau westward of Mesa Range and is wide, narrowing to near the coast. It takes its name from Rennick Bay where the glacier reaches the sea. The seaward part of the glacier was photographed by U.S. Navy (USN) Operation Highjump, 1946–47. The upper reaches of the Rennick Glacier were discovered and explored by the U.S. Victoria Land Traverse (VLT) in February 1960, and the first ascent made of Welcome Mountain by John Weihaupt, Alfred Stuart, Claude Lorius and Arnold Heine of the VLT party. On February 10, 1960, Lieutenant Commander Robert L. Dale, pilot of U.S. Navy (USN) Squadron VX-6, evacuated the VLT from 7238S, 16132E, on this glacier, and then conducted an aerial photographic reconnaissance to Rennick Bay on the coast before returning the VLT team to McMurdo Station. Features * Illusion Hills, small hills on the glacier * Litell Rocks, an area of rock outcr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
