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Dryland Landscapes

Frost-shattered debris, nivation hollows and solifluction deposits

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  • Component 01

Overview

Recall questions on relict periglacial landforms in warm deserts, frost shattering and recognising its debris, relict scree slopes, nivation hollows and their aspect, solifluction and its deposits, and how warming affects periglacial features in drylands and polar deserts.

What you need to know

Answer each one before you reveal it.

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Key term

Why do some warm deserts contain landforms made by frost?

Key term

How does frost shattering break rock apart?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Why do some warm deserts contain landforms made by frost?

    Model answer

    During the cold stages of the Pleistocene these areas were far colder, so periglacial processes operated there, and the landforms they produced survive today as relict features.

  2. 2

    Define the term periglacial.

    Model answer

    Periglacial describes the cold conditions found beyond the margins of ice sheets and glaciers, where frost action and frozen ground rather than moving ice dominate the landscape.

  3. 3

    How does frost shattering break rock apart?

    Model answer

    Water held in a crack expands by about 9% as it freezes and forces the crack wider, and repeated cycles of freezing and thawing eventually split the rock into angular fragments.

  4. 4

    How can frost-shattered debris be recognised in the field?

    Model answer

    It consists of very angular, poorly sorted fragments with sharp unworn edges, usually forming a blocky sheet on flat ground or a scree at the foot of a rock face.

  5. 5

    How can you tell that a scree slope in a dryland is relict rather than active?

    Model answer

    The debris is stable and often cemented, and it is colonised by lichen, soil and plants, with no fresh angular material lying at the surface or newly fallen onto it.

  6. 6

    What is nivation?

    Model answer

    Nivation is the combination of frost weathering, chemical weathering and removal of debris by meltwater that operates beneath and around a patch of snow lying through the summer.

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