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Glaciated Landscapes

Geology, relief and aspect in glaciated landscapes

  • 3 things to know
  • Component 01

Overview

Recall questions on lithology and geological structure in glaciated landscapes, how jointing and weak or resistant rock bands shape erosion and troughs, the Skiddaw Slates and Borrowdale Volcanic rocks of the Lake District, and how relief and aspect decide where ice forms and why corries face north-east.

What you need to know

Answer each one before you reveal it.

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Key term

Define lithology as a control on glaciated landscapes

Key term

What is meant by geological structure in a glaciated landscape?

Key term

Explain how well-jointed rock increases the rate of glacial erosion.

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Define lithology.

    Model answer

    Lithology is the physical and chemical make-up of a rock, including its hardness, mineral content and how readily it is weathered.

  2. 2

    What is meant by geological structure in a glaciated landscape?

    Model answer

    Structure is the arrangement of the rock, including its joints, bedding planes, faults and the angle at which the strata dip.

  3. 3

    Why do resistant rocks such as granite produce craggy glaciated uplands?

    Model answer

    They erode slowly, so the ice removes the weaker rock around them and leaves steep, angular high ground standing above the valleys.

  4. 4

    Explain how well-jointed rock increases the rate of glacial erosion.

    Model answer

    Meltwater enters the joints and refreezes onto the blocks, so ice can pluck loose fragments away far more easily than it can break intact, massive rock.

  5. 5

    How does a band of weak rock crossing a valley floor affect the shape of a glacial trough?

    Model answer

    The ice erodes the weaker band more deeply, forming a rock basin that may later hold a ribbon lake.

  6. 6

    What happens where a bar of resistant rock crosses the floor of a glacial trough?

    Model answer

    It is eroded more slowly than the rock around it and is left as a step or threshold over which the valley floor drops steeply.

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