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Glaciated Landscapes and Change

What controls the rate of glacial movement

  • 3 things to know
  • Paper 1

Overview

How altitude, basal temperature, gradient, lithology, ice thickness and mass balance control the rate of glacial movement, positive and negative feedback in glacier flow, extending and compressing flow, calculating mass balance and the equilibrium line, and using GIS to map glacier zones and assess glacier health.

What you need to know

Answer each one before you reveal it.

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Process

How does basal temperature control whether basal slip can occur?

Key term

What is compressing flow and where does it occur?

Key term

How does higher altitude affect both accumulation and ablation rates?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    How does higher altitude affect both accumulation and ablation rates?

    Model answer

    Higher altitude increases accumulation due to lower temperatures and greater snowfall, while also reducing ablation.

  2. 2

    How does basal temperature control whether basal slip can occur?

    Model answer

    Temperatures at or above pressure melting point allow meltwater to form, providing lubrication for basal slip; temperatures below this prevent it.

  3. 3

    Why do steeper slopes increase the rate of glacial movement?

    Model answer

    Greater gravitational force acts on the ice mass, accelerating its downslope movement.

  4. 4

    How does lithology affect glacial movement rates?

    Model answer

    Rough, resistant bedrock increases friction and slows basal sliding, while smooth bedrock facilitates faster movement.

  5. 5

    Why do larger glaciers with greater ice thickness tend to move faster?

    Model answer

    Increased pressure at the base promotes pressure melting and basal slip, and greater weight drives internal deformation.

  6. 6

    How does a positive mass balance affect glacial movement rates?

    Model answer

    It increases ice thickness and pressure, which accelerates movement.

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