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Glaciated Landscapes

Glacial weathering and erosion processes

  • 3 things to know
  • AS Unit 1

Overview

Freeze-thaw weathering in a glacial environment, frost shattering and abrasion as a glacial process.

What you need to know

Answer each one before you reveal it.

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Key term

Describe freeze-thaw weathering in a glacial environment.

Key term

Why is freeze-thaw weathering so effective in glacial environments?

Process

Describe plucking as a glacial process.

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Describe freeze-thaw weathering in a glacial environment.

    Model answer

    Meltwater enters a crack in the rock and freezes as temperatures fall, expanding by about 9% and widening the crack, and repeated cycles shatter the rock into angular fragments.

  2. 2

    Why is freeze-thaw weathering so effective in glacial environments?

    Model answer

    Temperatures cross 0°C frequently, particularly in spring and autumn and on a daily cycle, and meltwater is abundant to fill the cracks.

  3. 3

    What is frost shattering, and what does it produce on a mountainside?

    Model answer

    Frost shattering is repeated freeze-thaw breaking rock apart, and it produces angular scree at the foot of the slope and blockfields on flatter ground.

  4. 4

    Describe abrasion as a glacial process.

    Model answer

    Rock fragments held in the base of the ice are dragged across the bedrock and scour it, in the way that sandpaper wears a surface.

  5. 5

    Describe plucking as a glacial process.

    Model answer

    Meltwater at the base freezes onto jointed bedrock, and as the glacier moves it pulls blocks of that rock away with it.

  6. 6

    Which glacial process requires meltwater at the bed, and why does that matter?

    Model answer

    Plucking, because the ice must freeze onto the rock, so it operates under warm-based glaciers and not where the bed is permanently frozen.

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