Mount Brennan
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Mount Brennan
Mount Brennan () is a dome-shaped mountain, high, which is the northernmost prominent summit in the Hughes Range, standing northeast of Mount Cartwright. It was discovered and photographed by the United States Antarctic Service on Flight C of February 29–March 1, 1940, and surveyed by A.P. Crary in 1957–58. It was named by Crary for Matthew J. Brennan, scientific station leader at Ellsworth Station Ellsworth Scientific Station ( es, Estación Científica Ellsworth, or simply ''Estación Ellsworth'' or ''Base Ellsworth'') was a permanent, all year-round originally American, then Argentine Antarctic scientific research station named after Amer ..., 1958. References Mountains of the Ross Dependency Dufek Coast {{DufekCoast-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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