Mount Reid
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Mount Reid
Mount Reid () is a prominent, mainly ice-free mountain, 3,315 m, standing just east of the head of Cleaves Glacier in the Holland Range The Holland Range () is a rugged coastal mountain range in Antarctica, about long, lying just west of the Ross Ice Shelf and extending from Robb Glacier to Lennox-King Glacier. It was named by the Ross Sea Committee for Sir Sidney Holland, who as .... Discovered by the British Antarctic Expedition (1907–09) and named for Alfred Reid, manager of the expedition. Mountains of the Ross Dependency Shackleton Coast {{ShackletonCoast-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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Cleaves 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 (NZGSAE) (1959–60), who traversed this glacier to reach Lowery Glacier. See also *Cape Huinga *Whakawhiti Saddle *Worthley Peak Worthley Peak () is a peak, 840 m, at the north end of Benson Ridge overlooking lower Robb Glacier. Mapped by the United States Geological Survey (USGS) from tellurometer surveys and Navy air photos, 1960–62. Named by Advisory Committee on A ... References Glaciers of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ...
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Holland Range
The Holland Range () is a rugged coastal mountain range in Antarctica, about long, lying just west of the Ross Ice Shelf and extending from Robb Glacier to Lennox-King Glacier. It was named by the Ross Sea Committee for Sir Sidney Holland, who as Prime Minister of New Zealand supported that nation's participation in 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). References Mountain ranges of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ...
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British Antarctic Expedition, 1907–09
The ''Nimrod'' Expedition of 1907–1909, otherwise known as the British Antarctic Expedition, was the first of three successful expeditions to the Antarctic led by Ernest Shackleton and his second expedition to the Antarctic. Its main target, among a range of geographical and scientific objectives, was to be first to the South Pole. This was not attained, but the expedition's southern march reached a Farthest South latitude of 88° 23' S, just from the pole. This was by far the longest southern polar journey to that date and a record convergence on either Pole. A separate group led by Welsh Australian geology professor Edgeworth David reached the estimated location of the South Magnetic Pole, and the expedition also achieved the first ascent of Mount Erebus, Antarctica's second highest volcano. The expedition lacked governmental or institutional support, and relied on private loans and individual contributions. It was beset by financial problems and its preparation ...
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Mountains Of The Ross Dependency
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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