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Landscapes of the UK

Geomorphic processes: weathering, mass movement, erosion, transport and deposition

  • 3 things to know
  • Component 01

Overview

Weathering against erosion, freeze-thaw, chemical and biological weathering, mass movement, sliding and slumping, abrasion, hydraulic action, attrition and solution, traction, saltation and suspension, and why deposition takes place.

What you need to know

Answer each one before you reveal it.

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Key term

What is mass movement, and how do sliding and slumping move material down a slope?

Key term

How do abrasion, hydraulic action and attrition each erode rock in a river or at the coast?

Key term

How does freeze-thaw, the main type of mechanical weathering, break up rock?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What is the difference between weathering and erosion?

    Model answer

    Weathering breaks rock down where it stands without moving it, while erosion wears rock away and carries the loosened material off.

  2. 2

    How does freeze-thaw, the main type of mechanical weathering, break up rock?

    Model answer

    Water collects in a crack and expands as it freezes below 0 °C, widening the crack, and repeated freezing and thawing eventually splits the rock apart.

  3. 3

    What happens during chemical weathering?

    Model answer

    Slightly acidic rainwater reacts with minerals in the rock and dissolves them, as when carbonation slowly eats away limestone.

  4. 4

    Give two ways living things cause biological weathering.

    Model answer

    Plant roots grow into cracks and prise the rock apart, and burrowing animals loosen and break up material.

  5. 5

    What is mass movement?

    Model answer

    The downhill movement of rock, soil and mud under gravity, often triggered when heavy rain makes the material heavier and more slippery.

  6. 6

    What happens when material slides down a slope?

    Model answer

    A mass of material moves rapidly straight downslope along a flat surface of weakness, keeping much of its original shape.

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