Cirque Floor Geology

Often the glaciers flow up and over the lip of the cirque as gravity drives them downslope.

Cirque floor geology.

Hence it experiences somewhat greater erosion forces and is most often overdeepened below the level of the cirque s low side outlet stage and its down slope backstage valley. Cirques are bowl shaped amphitheater like depressions that glaciers carve into mountains and valley sidewalls at high elevations. In early summer it opens exposing the rock at its base to diurnal. Geology a curved depression in a mountainside with steep walls forming the end of a valley.

Chapman and hall 193 piccadilly oclc 1561924. Cirques subjected to seasonal melting often form small lakes. Ticknor and fields 1856 oclc 187461130 stanzas 22. Circle amphitheatre shaped basin with precipitous walls at the head of a glacial valley it generally results from erosion beneath the bergschrund of a glacier a bergschrund is a large crevasse that lies a short distance from the exposed rock walls and separates the stationary from the moving ice.

True cirque growth only occurs once the thickness of snow patches increases to a point at which glacier ice can form by compaction. A cirque experiences greater erosion because of the accompanying rock burdens which may also over deepen the level of a cirque. Once formed glaciers widen and deepen cirques by subglacial abrasion and quarrying of the hollow floor and lower headwall 3 see diagram below. Corrie combe cwm 1855 robert browning childe roland to the dark tower came in men and women london.

The floor of the cirque is bowl shaped because of the convergence zones of combining ice flows from a different direction and the debris accompanying them. Elias national park alaska sits in a classic bowl shaped cirque.