Cirque

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-[[Image:Cirque mountain.jpg|thumb|300px|A steep-walled '''[[mountain]]''' basin which usually forms the blunt end of a '''[[valley]]'''. (French for "circus.")]]+[[Image:Cirque mountain.jpg|thumb|300px|'''[[Cirque]]''' is a steep-walled '''[[mountain]]''' basin which usually forms the blunt end of a '''[[valley]]'''. (French for "circus.")]]
[[Image:Mtnglacier.jpg|thumb|300px]] [[Image:Mtnglacier.jpg|thumb|300px]]
-A steep-walled '''[[mountain]]''' basin which usually forms the blunt end of a '''[[valley]]'''. (French for "circus.")+'''[[Cirque]]''' is a steep-walled '''[[mountain]]''' basin which usually forms the blunt end of a '''[[valley]]'''. (French for "circus.")
The concave amphitheatre shape is open on the downhill side corresponding to the flatter area of the stage, while the cupped seating section is generally steep cliff-like '''[[slopes]]''' down which ice and glaciated debris combine and converge from the three or more higher sides. The concave amphitheatre shape is open on the downhill side corresponding to the flatter area of the stage, while the cupped seating section is generally steep cliff-like '''[[slopes]]''' down which ice and glaciated debris combine and converge from the three or more higher sides.
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-== Also See ==+== '''Also See''' ==
*'''[[Mountain]]''' *'''[[Mountain]]'''

Revision as of 11:31, 8 August 2011

Cirque is a steep-walled mountain basin which usually forms the blunt end of a valley. (French for "circus.")
Cirque is a steep-walled mountain basin which usually forms the blunt end of a valley. (French for "circus.")

Cirque is a steep-walled mountain basin which usually forms the blunt end of a valley. (French for "circus.")

The concave amphitheatre shape is open on the downhill side corresponding to the flatter area of the stage, while the cupped seating section is generally steep cliff-like slopes down which ice and glaciated debris combine and converge from the three or more higher sides.

The floor of the cirque ends up bowl shaped as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens, hence experiences somewhat greater erosion forces, and is most often scooped out somewhat below the level of cirque's low-side outlet (stage) and its down slope (backstage) valley.

If the cirque is subject to seasonal melting, the floor of the cirque most often forms a tarn (small lake) behind the Moraine and glacial till damming the outlet.


Also See

Reference

  • Wikipedia Cirque [1]



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