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Mount Bower
The Outback Nunataks () are a series of bare rock nunataks and mountains which are distributed over an area about long by wide. The group lies south of Emlen Peaks of the Usarp Mountains and west of Monument Nunataks and upper Rennick Glacier, adjacent to the featureless interior plateau. Exploration and naming The Outback Nunataks were discovered by the United States Victoria Land Traverse party, 1959–60, and mapped by United States Geological Survey (USGS) from surveys and United States Navy air photos, 1959–64. They were so named by the Advisory Committee on Antarctic Names (US-ACAN) for their remote position at the posterior side of the large mountain belt that extends from the Ross Sea to the interior ice plateau. Location The terrain to the west of the nunataks is a featureless expanse of the polar plateau. The Emlen Peaks of the Usarp Mountains and the Helliwell Hills are to the north. The Rennick Glacier, the Freyberg Mountains, the Monument Nunataks a ...
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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 78th parallel south, 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 Victoria of the United Kingdom, 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. History Early explorers of Victoria Land include James Clark Ross and Douglas Mawson. In 1979, scientists discovered a group of 309 Meteorite, meteorites in Antarctica, some of which were found near the Allan Hills in Victoria Land. The meteorites appeared to have undergone little change since they were formed at what scientists believe was the birth of the Solar System. In 1981, Lichen, lichens fo ...
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C72200s1 Ant
C7, C07 or C-7 may refer to: Vehicles (including military) * C-7 Caribou, a military transport aircraft * AEG C.VII, a World War I German armed reconnaissance aircraft * AGO C.VII, a World War I German reconnaissance aircraft * Albatros C.VII, a World War I German military reconnaissance aircraft * C-7, a United States Navy C class blimp and the first airship inflated with helium * Chevrolet Corvette (C7), the seventh generation of a sports car made by General Motors * Fokker C.VII, a 1928 Dutch reconnaissance seaplane * HMS ''C7'', a British Royal Navy C-class submarine * Sauber C7, a 1983 Group C prototype race car * USS ''Cincinnati'' (C-7), a United States Navy protected cruiser Science * Caldwell 7 (NGC 2403), a spiral galaxy in Camelopardalis Technology * Nokia C7-00, a touch screen mobile from Nokia * VIA C7, an IA-32 central processing unit by VIA Technologies * C7, an incandescent light bulb of the size typically used in nightlights and Christmas lighting usually ...
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Sequence Hills
Sequence Hills () is an escarpment-like hills on the west margin of the upper Rennick Glacier, about 7 nautical miles (13 km) northwest of Caudal Hills, Victoria Land. They provided the only good geological sequence in the area. Mapped and named by the northern party of 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 19 ... (NZGSAE), 1962–63. See also * Barren Bluff * Waring Bluff Hills of Victoria Land Pennell Coast {{VictoriaLand-geo-stub ...
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Rennick Névé
Rennick Glacier () is a 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. Early exploration The seaward part of the glacier was photographed by United States Navy 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 , on this glacier, and then conducted an aerial photographic reconnaissance to Rennick Bay on the coast before returning the VLT team to McMurdo Station. Course The Rennick Glacier rises to the east of the Tobin Mesa in t ...
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Mesa Range
The Mesa Range () is a range of flat-topped mesas comprising the Sheehan, Pain, Tobin and Gair Mesas, situated at the head of the Rennick Glacier in Victoria Land, Antarctica. It was given this descriptive name by the northern party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE) of 1962–63. Location The Gair, Tobin and Pain mesas are in the east side of the middle reach of the Rennick Glacier, and the Sheehan Mesa is on the west side. The Monument Nunataks are to the northwest, the Freyberg Mountains to the north, Half-ration Névé and the larger Evans Névé to the northeast, the Southern Cross Mountains to the east, and the Deep Freeze Range to the south. Sheehan Mesa . A prominent mesa standing west-northwest of Pain Mesa in the northwest part of Mesa Range. Named by the northern party of NZGSAE, 1962–63, for Maurice Sheehan, field assistant with this party. Silva Ridge . A ridge leading to the top of Sheehan Mesa, on the northeast sid ...
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Freyberg Mountains
The Freyberg Mountains () are a group of mountains in Victoria Land, Antarctica, bounded by the Rennick Glacier, Bowers Mountains, Black Glacier, and Evans Névé. They are west of the Victory Mountains and south of the Bowers Mountains. Name The Freyberg Mountains were named for New Zealand's most famous general, Bernard Freyberg, by the Northern Party of New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1963–64. Location The Freyberg Mountains lie to the east of the Rennick Glacier and to the south of the Bowers Mountains Bowers Mountains () is a group of north–south trending mountains in Antarctica, about long and wide, bounded by the coast on the north and by the Rennick Glacier, Canham Glacier, Black Glacier and Lillie Glacier in other quadrants. They are we .... The Canham Glacier defines their northwest limit. The Black Glacier defines their eastern limit, separating them from the Leitch Massif, Neall Massif and West Quartzite Range further ...
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Helliwell Hills
The Helliwell Hills () are a group of rocky hills and low mountains about long and wide in the Usarp Mountains of North Victoria Land, Antarctica. Location The Helliwell Hills are part of the Usarp Mountains of North Victoria Land, Antarctica. They are south of Gressitt Glacier and midway between Emlen Peaks to the west and the Morozumi Range to the east. They are south of the Daniels Range, on the other side of Gressitt Glacier, and north of the Outback Nunataks. Early exploration and name The Helliwell Hills were mapped by United States Geological Survey (USGS) from surveys and United States Navy air photos in 1960-63. They were named by the Advisory Committee on Antarctic Names (US-ACAN) for Robert A. Helliwell of Stanford University, Program Director for the USARP study of very low frequency (VLF) radio noise phenomena. Geology The cover rocks in the Helliwell Hills are Permian Beacon sediments and Jurassic Ferrar sills. The basement has low- to high-grade metamorphic ...
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C73202s5 Ant
C73 or C-73 may refer to : * Boeing C-73, a 1933 military aircraft * C-73 (Michigan county highway) * Ruy Lopez chess openings ECO code * Thyroid cancer Thyroid cancer is cancer that develops from the tissues of the thyroid gland. It is a disease in which cells grow abnormally and have the potential to spread to other parts of the body. Symptoms can include swelling or a lump in the neck, ... ICD-10 code * Caldwell 73 ( NGC 1851), a globular cluster in the constellation Columba {{Letter-NumberCombDisambig ...
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C72193s5 Ant
C7, C07 or C-7 may refer to: Vehicles (including military) * C-7 Caribou, a military transport aircraft * AEG C.VII, a World War I German armed reconnaissance aircraft * AGO C.VII, a World War I German reconnaissance aircraft * Albatros C.VII, a World War I German military reconnaissance aircraft * C-7, a United States Navy C class blimp and the first airship inflated with helium * Chevrolet Corvette (C7), the seventh generation of a sports car made by General Motors * Fokker C.VII, a 1928 Dutch reconnaissance seaplane * HMS ''C7'', a British Royal Navy C-class submarine * Sauber C7, a 1983 Group C prototype race car * USS ''Cincinnati'' (C-7), a United States Navy protected cruiser Science * Caldwell 7 (NGC 2403), a spiral galaxy in Camelopardalis Technology * Nokia C7-00, a touch screen mobile from Nokia * VIA C7, an IA-32 central processing unit by VIA Technologies * C7, an incandescent light bulb of the size typically used in nightlights and Christmas lighting usually ...
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Ross Sea
The Ross Sea is a deep bay of the Southern Ocean in Antarctica, between Victoria Land and Marie Byrd Land and within the Ross Embayment, and is the southernmost sea on Earth. It derives its name from the British explorer James Clark Ross who visited this area in 1841. To the west of the sea lies Ross Island and Victoria Land, to the east Roosevelt Island and Edward VII Peninsula in Marie Byrd Land, while the southernmost part is covered by the Ross Ice Shelf, and is about from the South Pole. Its boundaries and area have been defined by the New Zealand National Institute of Water and Atmospheric Research as having an area of . The circulation of the Ross Sea is dominated by a wind-driven ocean gyre and the flow is strongly influenced by three submarine ridges that run from southwest to northeast. The circumpolar deep water current is a relatively warm, salty and nutrient-rich water mass that flows onto the continental shelf at certain locations. The Ross Sea is covered ...
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Nunatak
A nunatak (from Inuit language, Inuit ) is the summit or ridge of a mountain that protrudes from an ice field or glacier that otherwise covers most of the mountain or ridge. They often form natural pyramidal peaks. Isolated nunataks are also called glacial islands, and smaller nunataks rounded by glacial action may be referred to as rognons. The word is of Greenlandic language, Greenlandic origin and has been used in English since the 1870s. Description The term ''nunatak'' is typically used in areas where a permanent ice sheet is present and the ridge protrudes above the sheet.J. J. Zeeberg, ''Climate and Glacial History of the Novaya Zemlya Archipelago, Russian Arctic''. pp. 82–84 Nunataks present readily identifiable landmark reference points in glaciers or ice caps and are often named. While some are isolated, they can also form dense clusters, such as Queen Louise Land in Greenland. Nunataks are generally angular and jagged, hampering the formation of glacial ice on thei ...
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