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Glaciated Landscapes

Warm-based and cold-based ice, and the mechanisms of glacier movement

  • 3 things to know
  • Component 01

Overview

Recall questions on warm-based and cold-based glaciers and the pressure melting point, basal sliding, regelation, enhanced basal creep and internal deformation, the velocity profile of a valley glacier, extending and compressing flow, crevasses, glacier surges and the effect of summer meltwater.

What you need to know

Answer each one before you reveal it.

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Key term

Name two sources of heat that can bring the base of a thick glacier to its pressure melting point.

Key term

Why is a cold-based glacier associated with very little erosion?

Key term

Compare typical rates of movement of warm-based and cold-based glaciers.

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What is a warm-based glacier?

    Model answer

    It is a glacier whose base is at the pressure melting point, so meltwater is present at the bed and the ice can slide over it.

  2. 2

    What is a cold-based glacier?

    Model answer

    It is a glacier whose base is well below the pressure melting point, so the ice is frozen to the bedrock and cannot slide.

  3. 3

    What is the pressure melting point?

    Model answer

    It is the temperature at which ice melts under a given pressure, and it falls below 0 °C as the weight of overlying ice increases.

  4. 4

    Name two sources of heat that can bring the base of a thick glacier to its pressure melting point.

    Model answer

    Geothermal heat rising from the rock beneath and frictional heat generated as the ice moves over its bed.

  5. 5

    Why is a cold-based glacier associated with very little erosion?

    Model answer

    The ice is frozen to its bed and moves almost entirely by internal deformation, so debris is not dragged across the rock and abrasion and plucking barely occur.

  6. 6

    Compare typical rates of movement of warm-based and cold-based glaciers.

    Model answer

    Warm-based glaciers commonly move tens to hundreds of metres a year, while cold-based glaciers may move only a few metres a year.

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