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Glacial Systems and Landscapes

Periglacial Landforms and Processes

  • 4 things to know
  • Component 1

Overview

Recall questions on how frost heave forms patterned ground, stone circles and stripes, on ice wedges, open- and closed-system pingos and blockfields, and on the active layer, permafrost and solifluction with its lobes and terracettes.

What you need to know

Answer each one before you reveal it.

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Key term

What repeated process drives the formation of patterned ground in periglacial environments?

Key term

What causes the initial crack that begins ice-wedge formation?

Key term

What structural feature gives a pingo its dome shape?

Process

Explain how frost heave and slope angle produce patterned ground.

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What repeated process drives the formation of patterned ground in periglacial environments?

    Model answer

    Repeated freeze-thaw cycles cause frost heave and sorting of surface material.

  2. 2

    Explain how frost heave contributes to patterned ground development.

    Model answer

    Frost heave pushes larger stones upward through the soil as ice lenses grow, bringing coarse material to the surface.

  3. 3

    How do stones become arranged into polygons or stripes in patterned ground?

    Model answer

    After being heaved to the surface, stones migrate laterally through repeated freeze-thaw, accumulating at the edges of sorted patterns.

  4. 4

    Under what slope conditions do stone circles form, and when do stone stripes develop instead?

    Model answer

    Stone circles form on flat or gently sloping ground; stone stripes develop on steeper slopes where gravity elongates the patterns.

  5. 5

    What causes the initial crack that begins ice-wedge formation?

    Model answer

    Extreme winter cold causes thermal contraction of the frozen ground, opening a vertical crack in the permafrost.

  6. 6

    What fills the crack in permafrost during spring, and what happens to it?

    Model answer

    Spring meltwater enters the crack and refreezes, adding a thin layer of ice to the wedge.

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AThe horns have less sand volume, so they move more quickly.
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Weathering means breakdown of rock in place.
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