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Glaciated Landscapes

Ice-contact fluvioglacial landforms

  • 2 things to know
  • Component 1 Section A

Overview

How an esker forms, how a delta kame forms and how a kame terrace forms.

What you need to know

Answer each one before you reveal it.

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Key term

Define an esker.

Key term

Explain how an esker forms.

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Define an esker.

    Model answer

    An esker is a long, sinuous ridge of sorted sand and gravel. The ridge can run for tens of kilometres and stands 5 m to 30 m high.

  2. 2

    Explain how an esker forms.

    Model answer

    Meltwater flows under pressure through a tunnel at the base of the glacier and deposits its load on the tunnel floor. The ice walls are removed when the glacier melts, leaving the channel fill standing as a ridge.

  3. 3

    Why can an esker run uphill?

    Model answer

    Water in a subglacial tunnel is under hydrostatic pressure from the ice above. Pressure can drive the flow up a gentle slope, so the ridge follows the ice surface gradient rather than the ground.

  4. 4

    How can an esker be recognised from its sediment?

    Model answer

    Esker sediment is rounded, sorted and stratified, unlike the till around it. Cross-bedding within it shows the direction the meltwater flowed.

  5. 5

    Give a named esker.

    Model answer

    The Trim esker in County Meath, Ireland, runs for about 14 km. Long eskers are also common across the Canadian Shield.

  6. 6

    Define a kame.

    Model answer

    A kame is an isolated mound of stratified sand and gravel. The mound is typically 10 m to 50 m high with steep, irregular sides.

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