Mount Shadow
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Mount Shadow
Mount Shadow () is a small Summit (topography), peak in the Admiralty Mountains that rises above and close west of Shadow Bluff at the junction of the Tucker and Leander Glaciers. Climbed by the geological team of the New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1957–58, in January 1958, and named from association with Shadow Bluff and nearby Mount Midnight. Admiralty Mountains Mountains of Victoria Land Borchgrevink Coast {{BorchgrevinkCoast-geo-stub ...
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Summit (topography)
A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. The topographic terms acme, apex, peak (mountain peak), and zenith are synonymous. The term (mountain top) is generally used only for a mountain peak that is located at some distance from the nearest point of higher elevation. For example, a big, massive rock next to the main summit of a mountain is not considered a summit. Summits near a higher peak, with some prominence or isolation, but not reaching a certain cutoff value for the quantities, are often considered ''subsummits'' (or ''subpeaks'') of the higher peak, and are considered part of the same mountain. A pyramidal peak is an exaggerated form produced by ice erosion of a mountain top. Summit may also refer to the highest point along a line, trail, or route. The highest summit in the world is Mount Everest with a height of above sea level. The first official ascent was made by Tenzing Norgay and Sir Edmund Hillary ...
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Admiralty Mountains
The Admiralty Mountains (alternatively Admiralty Range) is a large group of high mountains and individually named ranges and ridges in northeastern Victoria Land, Antarctica. This mountain group is bounded by the Ross Sea, the Southern Ocean, and by the Dennistoun, Ebbe, and Tucker glaciers. The mountain range is situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare. It was discovered in January 1841 by Captain James Ross, who named them for the Lords Commissioners of the Admiralty under whose orders he served. The Admiralty Mountains are divided into the Dunedin Range, Homerun Range, and Lyttelton Range. Mountains and peaks This range includes the following mountains and peaks: Mount Achilles Mount Achilles is a prominent pyramidal mountain rising from the divide between Fitch Glacier and Man-o-War Glacier. Named by New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1957–58, after the former New Zealand cruiser ...
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Shadow Bluff
Shadow Bluff () is a rock bluff in Antarctica, just west of McGregor Range, at the junction of the Tucker and Leander Glaciers. It is a landmark when sledging on the Tucker Glacier, and is nearly always in shadow, hence the name. Named by 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), 1957–58. Cliffs of Victoria Land Borchgrevink Coast {{BorchgrevinkCoast-geo-stub ...
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Leander Glacier
Leander Glacier () is a tributary glacier in the Admiralty Mountains of Antarctica, draining the area west of Mount Black Prince and flowing south between Shadow Bluff and the McGregor Range to enter Tucker Glacier. It was partially surveyed by the New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1957–58, which also observed the upper parts of the glacier from Mount Midnight and Mount Shadow. It was named by the NZGSAE for the light cruiser HMNZS ''Leander'' which served in World War II World War II or the Second World War, often abbreviated as WWII or WW2, was a world war that lasted from 1939 to 1945. It involved the vast majority of the world's countries—including all of the great powers—forming two opposing .... See also * Pemmican Step References Glaciers of Borchgrevink Coast {{BorchgrevinkCoast-glacier-stub ...
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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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Mount Midnight
Mount Midnight is a peak nearly high, standing on the north side of Tucker Glacier, west of Shadow Bluff, in the Admiralty Mountains of Antarctica. It was climbed by a geological team of the New Zealand Geological Survey Antarctic Expedition in January 1958, and was named by them in association with Mount Shadow Mount Shadow () is a small Summit (topography), peak in the Admiralty Mountains that rises above and close west of Shadow Bluff at the junction of the Tucker and Leander Glaciers. Climbed by the geological team of the New Zealand Geological Surve ..., just eastward, and Shadow Bluff. References Mountains of Victoria Land Borchgrevink Coast {{BorchgrevinkCoast-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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