Erosion formations
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Pictures say a thousand words and this diagram shows how the cirque is formed.
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This is a U shaped valley that typically have steep sides and flat floors. The glacier widens, steepens, deepens and smooths pre-existing V-shaped river valley.
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When a river erodes the landscape, ridges of land form in its upper course which jut into the river. These are called interlocking spurs. A glacier cuts through these ridges leaving behind truncated spurs
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An arête is a knife-edge ridge. It is formed when two neighbouring corries run back to back. As each glacier erodes either side of the ridge, the edge becomes steeper and the ridge becomes narrower, eg Striding Edge found on Helvellyn in the Lake District. (BBC bitesize)
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A pyramidal peak is formed where three or more corries and arêtes meet. The glaciers have carved away at the top of a mountain, creating a sharply pointed summit, eg Mont Blanc, The Matterhorn and Mount Everest. (BBC bitesize)
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Other formations develop such as ribbon lakes that occur after the glacial has melted, they are often deep and flat bottomed. Roches moutonnée and Crag and tail are formations that develop when there is a change in the type of rock that the glacier passes over.
The erosional formations can create dramatic scenery and exciting places to visit often in National Parks.
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