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Glaciated Landscapes

Weathering, mass movement and nivation in cold environments

  • 3 things to know
  • Component 01

Overview

Recall questions on frost shattering and freeze-thaw, blockfields, pressure release and chemical weathering in cold environments, scree slopes, rockfall after glacier retreat, solifluction and avalanches, and how nivation deepens a hollow into the first stage of a corrie.

What you need to know

Answer each one before you reveal it.

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Key term

What is frost shattering?

Key term

What conditions make freeze-thaw weathering most effective?

Key term

What is pressure release weathering?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What is frost shattering?

    Model answer

    Water in a crack freezes and expands, widening the crack, and repeated cycles break the rock into angular fragments.

  2. 2

    By roughly what percentage does water expand when it freezes?

    Model answer

    About 9%.

  3. 3

    What conditions make freeze-thaw weathering most effective?

    Model answer

    Frequent temperature swings across 0 °C, a reliable supply of water and well-jointed rock.

  4. 4

    Where in a glaciated valley would you expect freeze-thaw weathering to be most active?

    Model answer

    On exposed rock faces above the ice, such as corrie back walls and the crags above a trough, where both water and repeated frost are available.

  5. 5

    What is a blockfield?

    Model answer

    It is an expanse of large angular boulders produced in place by frost shattering, typically on an exposed plateau summit.

  6. 6

    What is pressure release weathering?

    Model answer

    When thick ice or overlying rock is removed, the reduction in pressure allows the rock beneath to expand and crack along joints running parallel to the surface.

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