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Navarro Ridge) is a rugged ridge in Antarctica, 3.5 nautical miles (6.5 km) long, that extends from the Coombs Hills southeastward to the west side of Cambridge Glacier The central peak of the ridge rises to 2,100 metres (6,900 ft).
An arête is a thin ridge of rock that is formed by glacial erosion. [2] Pressure ridge (ice) An ice pressure ridge is a ridge of deformed ice along the boundaries of individual ice floes when the ice floes on a lake or ocean collide and compress their edges. The average height of a sea ice pressure ridge is between 5 and 30 meters. [8]
[5] crevasse 1. A deep crack, fissure, or chasm in the ice of a glacier or ice sheet, or more generally in any ground surface. 2. A break in the natural levee or bank of a river. [4] crust The thin shell of solid material that is the Earth's outermost layer and the outermost component of the lithosphere.
[5] The crests of the Great Dividing Range is defined by the watershed boundary between the drainage basins of river systems east (the coastal or rainward side) and west (the inland or leeward side) of it. The higher and more rugged parts of the "range" do not necessarily form part of the crest of the range, but may be branches and offshoots ...
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Additionally, soil loss contributes to pollution, flooding, and sedimentation of waterways. [5] The formation of ravine lands can be sped up by deforestation and overgrazing . [ 6 ] In Indian badlands , soil erosion is estimated to exceed a rate of 40 tonnes per hectare (16 long ton/acre; 18 short ton/acre) annually.
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An abyssal plain is an underwater plain on the deep ocean floor, usually found at depths between 3,000 and 6,000 metres (9,800 and 19,700 ft).Lying generally between the foot of a continental rise and a mid-ocean ridge, abyssal plains cover more than 50% of the Earth's surface.
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