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Welcome Mountain
Welcome Mountain () is a very prominent 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 ... that is surmounted by three peaks, the highest 2,505 m, standing 5 nautical miles (9 km) southeast of Mount Southard in the Outback Nunataks. Discovered and named by the U.S. Victoria Land Traverse party, 1959–60. So named because it was the first mountain visited by the traverse party after crossing the interior plateau and not seeing any mountains or landmark features for nearly three months. Further reading * Gunter Faure, Teresa M. Mensing, 'The Transantarctic Mountains: Rocks, Ice, Meteorites and Water'', PP 109 - 110 * Edmund Stump, 'The Ross Orogen of the Transantarctic Mountains'', PP 17-18 External links USGC mapWelcome Mountain at the SCAR Composite Gazet ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
C72200s1 Ant
C7, C07 or C-7 may refer to: Vehicles (including military) * C-7 Caribou, a military transport aircraft * AEG C.VII, a World War I German armed reconnaissance aircraft * AGO C.VII, a World War I German reconnaissance aircraft * Albatros C.VII, a World War I German military reconnaissance aircraft * C-7, a United States Navy C class blimp and the first airship inflated with helium * Chevrolet Corvette (C7), the seventh generation of a sports car made by General Motors * Fokker C.VII, a 1928 Dutch reconnaissance seaplane * HMS ''C7'', a British Royal Navy C-class submarine * Sauber C7, a 1983 Group C prototype race car * USS ''Cincinnati'' (C-7), a United States Navy protected cruiser Science * Caldwell 7 (NGC 2403), a spiral galaxy in Camelopardalis Technology * Nokia C7-00, a touch screen mobile from Nokia * VIA C7, an IA-32 central processing unit by VIA Technologies * C7, an incandescent light bulb of the size typically used in nightlights and Christmas lighting usually 2 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Southard
Outback Nunataks () is a series of bare rock nunataks and mountains which are distributed over an area about long by wide. The group lies south of Emlen Peaks of the Usarp Mountains and west of Monument Nunataks and upper Rennick Glacier, adjacent to the featureless interior plateau. They were discovered by the U.S. Victoria Land Traverse party, 1959–60, and mapped by United States Geological Survey (USGS) from surveys and U.S. Navy air photos, 1959–64. They were so named by Advisory Committee on Antarctic Names (US-ACAN) for their remote position at the posterior side of the large mountain belt that extends from the Ross Sea to the interior ice plateau. Features Geographic features of the Outback Nunataks include: * Chan Rocks * Coleman Bluffs * De Camp Nunatak * Derbyshire Peak * Doe Nunatak * Doescher Nunatak * Fitzsimmons Nunataks * Frontier Mountain * Johannessen Nunataks * Miller Butte * Mount Blair * Mount Bower * Mount Chadwick * Mount Joern * Mount ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Outback Nunataks
Outback Nunataks () is a series of bare rock nunataks and mountains which are distributed over an area about long by wide. The group lies south of Emlen Peaks of the Usarp Mountains and west of Monument Nunataks and upper Rennick Glacier, adjacent to the featureless interior plateau. They were discovered by the U.S. Victoria Land Traverse party, 1959–60, and mapped by United States Geological Survey (USGS) from surveys and U.S. Navy air photos, 1959–64. They were so named by Advisory Committee on Antarctic Names (US-ACAN) for their remote position at the posterior side of the large mountain belt that extends from the Ross Sea to the interior ice plateau. Features Geographic features of the Outback Nunataks include: * Chan Rocks * Coleman Bluffs * De Camp Nunatak * Derbyshire Peak * Doe Nunatak * Doescher Nunatak * Fitzsimmons Nunataks * Frontier Mountain * Johannessen Nunataks * Miller Butte * Mount Blair * Mount Bower * Mount Chadwick * Mount Joern * Mount ... [...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] |
