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Glaciated Landscapes

Glacial erosion and the marks it leaves on rock

  • 3 things to know
  • Component 01

Overview

Recall questions on abrasion and plucking, rock flour and striations, reading ice direction from roches moutonnées, crag and tail, whalebacks, knock and lochan topography, erosion by subglacial meltwater, and why thicker ice erodes faster.

What you need to know

Answer each one before you reveal it.

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Key term

Name three conditions needed for effective abrasion.

Key term

What is plucking?

Key term

Why is plucking most effective on well-jointed rock?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What is abrasion?

    Model answer

    It is the wearing away of bedrock by rock debris held in the base of the ice and dragged across the surface, acting like sandpaper.

  2. 2

    Name three conditions needed for effective abrasion.

    Model answer

    Debris-rich basal ice, a glacier that is sliding over its bed, and enough ice thickness to press the debris against the rock.

  3. 3

    What is plucking?

    Model answer

    Meltwater freezes onto jointed bedrock and, as the glacier moves on, blocks are torn away and carried off with the ice.

  4. 4

    Why is plucking most effective on well-jointed rock?

    Model answer

    The joints already divide the rock into blocks, so the ice needs only to freeze on and pull them out rather than break intact rock apart.

  5. 5

    What is rock flour?

    Model answer

    It is the very fine, silt-sized rock powder produced by abrasion, which gives meltwater streams and glacial lakes their milky, turquoise colour.

  6. 6

    What are striations?

    Model answer

    They are scratches and grooves cut into bedrock by angular debris dragged across it in the base of a glacier.

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