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Glaciated Landscapes

Glacio-fluvial landforms of deglaciation: kames, eskers and outwash plains

  • 2 things to know
  • Component 01

Overview

Recall questions on glacio-fluvial processes and deposits after the last glacial period, eskers, kames and kame terraces, outwash plains such as Skeiðarársandur in Iceland, jökulhlaups, kettle holes, and how these landforms are changing today.

What you need to know

Answer each one before you reveal it.

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Key term

Describe the climate change that ended the last glacial period in Britain.

Process

How did post-glacial warming change the dominant geomorphic process in a deglaciating landscape?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What does the term glacio-fluvial mean?

    Model answer

    It describes material deposited or landforms shaped by meltwater flowing from a glacier, rather than by the ice itself.

  2. 2

    Describe the climate change that ended the last glacial period in Britain.

    Model answer

    Temperatures rose sharply from about 11,700 years ago, ending the last cold snap and causing the rapid melting of the remaining ice.

  3. 3

    How did post-glacial warming change the dominant geomorphic process in a deglaciating landscape?

    Model answer

    Direct glacial erosion and deposition gave way to enormous volumes of meltwater, so sorting, fluvial transport and glacio-fluvial deposition took over.

  4. 4

    How can glacio-fluvial deposits be recognised in the field?

    Model answer

    They are sorted by size into distinct layers and their stones have been rounded by water transport.

  5. 5

    What is an esker?

    Model answer

    It is a long, winding ridge of sorted sand and gravel deposited by a stream flowing in a tunnel beneath or within the ice.

  6. 6

    Why can an esker run uphill across the landscape?

    Model answer

    The meltwater in the tunnel was under hydrostatic pressure from the weight of ice above it, so it could be forced up gradients.

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