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Mount Stearns
Mount Dromedary ( is a hump-shaped mountain, over high, standing east of Mount Kempe Mount Kempe () is a peak, high, midway between Mount Huggins and Mount Dromedary in the Royal Society Range of Victoria Land, Antarctica. It was discovered by the British National Antarctic Expedition (1901–04) which named it for Sir Alfred Br ... in the Royal Society Range of Victoria Land, Antarctica. First mapped by the BrNAE, 1901–04, but named by the BrAE, 1910–13. Named for the appearance of the mountain which resembles a dromedary's hump. References Sources * Mountains of Victoria Land Scott Coast {{ScottCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Kempe
Mount Kempe () is a peak, high, midway between Mount Huggins and Mount Dromedary in the Royal Society Range of Victoria Land, Antarctica. It was discovered by the British National Antarctic Expedition (1901–04) which named it for Sir Alfred Bray Kempe, at that time Treasurer of the Royal Society. Auster Pass is a high pass between Mount Huggins Mount Huggins () is a large conical mountain, high, surmounting the heads of Allison Glacier, Dale Glacier, and Potter Glacier in the Royal Society Range of Antarctica. It was discovered by the British National Antarctic Expedition (1901–04) ... and Mount Kempe. References Mountains of Victoria Land Scott Coast {{ScottCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
