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Glaciated Landscapes

Periglacial ground ice and permafrost features

  • 2 things to know
  • Component 1 Section A

Overview

Active layer, periglacial environment and ice lens.

What you need to know

Answer each one before you reveal it.

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Key term

Define permafrost.

Key term

Distinguish continuous, discontinuous and sporadic permafrost.

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Define permafrost.

    Model answer

    Permafrost is ground that stays at or below 0 °C for at least two consecutive years. Around a quarter of the northern hemisphere land surface is underlain by it.

  2. 2

    Distinguish continuous, discontinuous and sporadic permafrost.

    Model answer

    Continuous permafrost underlies over 90% of the surface in the coldest areas and can be 1,500 m thick in Siberia. Discontinuous permafrost has thawed patches and sporadic permafrost survives only in isolated pockets.

  3. 3

    What is the active layer?

    Model answer

    The active layer is the surface layer that thaws each summer and refreezes each winter. Depth ranges from a few centimetres to about 4 m.

  4. 4

    Why does the active layer become waterlogged in summer?

    Model answer

    Frozen ground beneath the active layer is impermeable, so meltwater cannot drain downward. The thawed surface becomes saturated and mobile.

  5. 5

    Define a periglacial environment.

    Model answer

    A periglacial environment is a cold region beyond the ice margin where frost processes dominate. Permafrost and a seasonally thawing active layer are its defining features.

  6. 6

    What is an ice lens?

    Model answer

    An ice lens is a horizontal body of segregated ice within the soil. Water is drawn towards the freezing front by capillary action and adds to the lens.

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