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Glaciated Landscapes

Corries, arêtes and pyramidal peaks

  • 3 things to know
  • Component 01

Overview

Recall questions on the shape and formation of corries, rotational slip, bergschrunds, rock lips and tarns such as Red Tarn on Helvellyn, arêtes such as Striding Edge, pyramidal peaks such as the Matterhorn, cols, and mapping corrie orientation with a chi-squared test.

What you need to know

Answer each one before you reveal it.

Your recallNot started
Key term

Give the Welsh and French terms for a corrie.

Key term

Name a corrie tarn on Helvellyn in the Lake District.

Key term

What is the typical ratio of a corrie's length to its height?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Describe the shape of a corrie.

    Model answer

    It is a deep, armchair-shaped hollow with a steep back wall, an over-deepened rock basin and a raised lip or threshold at its outer edge.

  2. 2

    Give the Welsh and French terms for a corrie.

    Model answer

    A cwm in Wales and a cirque in France.

  3. 3

    Explain the part played by rotational slip in deepening a corrie.

    Model answer

    The ice pivots along a curved path as it moves out of the hollow, pressing hardest in the middle of the basin and abrading it far deeper than the lip.

  4. 4

    How is the steep back wall of a corrie kept steep?

    Model answer

    Plucking removes blocks from the base of the wall and freeze-thaw shatters the rock above the ice, so the wall is constantly undercut and retreats.

  5. 5

    What is a bergschrund?

    Model answer

    It is the large crevasse that opens where the moving corrie ice pulls away from the ice frozen to the back wall.

  6. 6

    Why does a rock lip develop at the exit of a corrie?

    Model answer

    The rotating ice is thinner there and presses less firmly on the bed, so it erodes the rock less than in the deep basin behind.

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