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Coastal Landscapes

Lithology, geological structure and the plan of the coast

  • 3 things to know
  • Component 01

Overview

Recall questions on lithology and geological structure, how clay, chalk, granite and glacial till resist the sea, discordant and concordant coastlines around Swanage, how coves form, how the dip of the strata shapes a cliff profile, and why faults and joints become caves and geos.

What you need to know

Answer each one before you reveal it.

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Key term

Why do chalk cliffs stand almost vertically even though chalk is a fairly weak rock?

Key term

Explain why unconsolidated glacial till erodes far faster than the chalk beside it.

Key term

Define lithology as it affects the coast

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Define lithology.

    Model answer

    The physical and chemical make-up of a rock, including its mineral composition and how strongly its particles are cemented together.

  2. 2

    What is meant by geological structure at the coast?

    Model answer

    The arrangement of the rocks, including their bedding, jointing, faulting and the angle at which the strata dip.

  3. 3

    Why does clay retreat quickly under wave attack?

    Model answer

    Its particles are weakly bonded and it loses much of its strength when saturated, so waves remove it easily and it slumps readily.

  4. 4

    Why do chalk cliffs stand almost vertically even though chalk is a fairly weak rock?

    Model answer

    Chalk is permeable and well jointed, so water drains through it rather than building up pressure, and the joints give clean vertical failure surfaces.

  5. 5

    Why is granite highly resistant at the coast?

    Model answer

    It is a crystalline rock of interlocking crystals with few bedding planes, so there are far fewer lines of weakness for waves to exploit.

  6. 6

    What is a discordant coastline?

    Model answer

    A coast where bands of rock of differing resistance meet the sea at a high angle, so alternating headlands and bays develop.

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AThe lower quartile is the 2nd value, 11 cm.
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