Glaciers shape the land through processes of weathering, erosion, transportation and deposition, creating distinct landforms. A bowl-shaped hollow area formed by glaciation, sometimes containing...

Corries are hollows formed by glacial erosion, freeze-thaw weathering and rotational slip (a kind of landslide that occurs in concave-up, or basin-shaped, surfaces). Corries are where glaciers start to form. A corrie can also be referred to as a cirque (pronounced serk – …

A corrie is an armchair-shaped hollow found on the side of a mountain. This is where a glacier, a massive river of flowing ice, forms. Glaciers form the corrie when more and more snow piles up.

Oct 5, 2020 · Once formed, glaciers widen and deepen cirques by subglacial abrasion and quarrying of the hollow floor and lower headwall 3 (see diagram below). Cirques can also grow by backwards headwall erosion (wear back) due to frost-action, free-thaw, and mass movement 3,10.

Jan 6, 2025 · Learn about the formation of glacial landforms from corries to troughs, along with examiner tips and worked examples for the AQA GCSE Geography exam.

Sep 12, 2011 · One example of a glacial landform is a Corrie. Figure 2: Diagram illustrating the formaton of a Corrie (Source: Reference) A corrie is an amphitheatre shaped rock hollow and has a steep back wall with a deepened basin. It is often …

Corrie is a bowl shaped depression on the side of a mountain. Formed by abrasion and plucking. Glacier moves downslope, making the hole deeper. Plucking works on the back wall and makes it steeper. Rocks from the back wall may fall under the glacier and be used as a tool of abrasion.

Start studying Formation of a Corrie (Higher Geography Lithosphere). Learn vocabulary, terms and more with flashcards, games and other study tools.

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Start studying Formation of a Corrie. Learn vocabulary, terms and more with flashcards, games and other study tools.