Sculpture Mountain
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Sculpture Mountain
Sculpture Mountain () is a large dissected mountain between the Monument Nunataks and Sheehan Mesa. Named by the Northern Party of New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1962–63, due to the cuspate embayment A bay is a recessed, coastal body of water that directly connects to a larger main body of water, such as an ocean, a lake, or another bay. A large bay is usually called a gulf, sea, sound, or bight. A cove is a small, circular bay with a narr ... which has been sculptured into the feature. The mountain is at the end of the Mesa Range and was renamed from Sculpture Tableland to the feature's current name when its status as a mountain was confirmed. Cherry Spur forms the southwest portion of the mountain, while Tooth Peak is in the north face. References Mountains of Victoria Land Pennell Coast {{VictoriaLand-geo-stub ...
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Mountain
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 (topography), 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 Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, 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 Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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Monument Nunataks
The Monument Nunataks () are a group of nunataks in Antarctica that have numerous pinnacles and odd-shaped projections resembling monuments, situated at the northern extremity of the Mesa Range, north of Sculpture Mountain in the upper part of Rennick Glacier. The group was named by the Northern Party 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 ... of 1962–63. References Nunataks of Victoria Land Pennell Coast {{VictoriaLand-geo-stub ...
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Sheehan Mesa
Sheehan Mesa () is a prominent mesa standing 10 miles (16 km) west-northwest of Pain Mesa in the northwest part of Mesa Range, Victoria Land. 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 1957 ... (NZGSAE), 1962–63, for Maurice Sheehan, field assistant with this party. References Mesas of Antarctica Mountains of Victoria Land Pennell Coast {{VictoriaLand-geo-stub ...
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Northern Party
The Northern Party was a regionalist political party in Northern England, founded by leader Michael Dawson and former Blackpool MP Harold Elletson in March 2015 to contest five marginal seats in Lancashire at the 2015 general election. The party was one of three regionalist parties contesting the general election in the north of England. Members included former activists from the Conservative, Labour, Liberal Democrat and Green parties. Founding Michael Dawson, a former Executive Committee member of the Labour Campaign for Human Rights, is the nephew of former MP for Lancaster Hilton Dawson who now runs the North East Party. At the launch of the party he said "We've been planning this for months. This is a Northern rebellion against a system that has failed the North." The party argued for Northern England devolution of power to an autonomous Northern region, and for business investment and environmental protection. The party described its symbol as "a Norse raven, closely as ...
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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 ...
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Embayment
A bay is a recessed, coastal body of water that directly connects to a larger main body of water, such as an ocean, a lake, or another bay. A large bay is usually called a gulf, sea, sound, or bight. A cove is a small, circular bay with a narrow entrance. A fjord is an elongated bay formed by glacial action. A bay can be the estuary of a river, such as the Chesapeake Bay, an estuary of the Susquehanna River. Bays may also be nested within each other; for example, James Bay is an arm of Hudson Bay in northeastern Canada. Some large bays, such as the Bay of Bengal and Hudson Bay, have varied marine geology. The land surrounding a bay often reduces the strength of winds and blocks waves. Bays may have as wide a variety of shoreline characteristics as other shorelines. In some cases, bays have beaches, which "are usually characterized by a steep upper foreshore with a broad, flat fronting terrace".Maurice Schwartz, ''Encyclopedia of Coastal Science'' (2006), p. 129. Bays were sig ...
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Cherry Spur
The Monument Nunataks () are a group of nunataks in Antarctica that have numerous pinnacles and odd-shaped projections resembling monuments, situated at the northern extremity of the Mesa Range, north of Sculpture Mountain in the upper part of Rennick Glacier. The group was named by the Northern Party 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 ... of 1962–63. References Nunataks of Victoria Land Pennell Coast {{VictoriaLand-geo-stub ...
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Tooth Peak
The Monument Nunataks () are a group of nunataks in Antarctica that have numerous pinnacles and odd-shaped projections resembling monuments, situated at the northern extremity of the Mesa Range, north of Sculpture Mountain in the upper part of Rennick Glacier. The group was named by the Northern Party 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 ... of 1962–63. References Nunataks of Victoria Land Pennell Coast {{VictoriaLand-geo-stub ...
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Mountains Of Victoria Land
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 ...
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