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Coastal Landscapes

Cliffs, wave-cut platforms, geos and blowholes

  • 2 things to know
  • Component 1 Section A

Overview

Formation of a cliff, formation of a wave-cut platform and typical gradient of a wave-cut platform.

What you need to know

Answer each one before you reveal it.

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Key term

Describe the formation of a cliff.

Key term

Why does a cliff retreat parallel to itself?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Describe the formation of a cliff.

    Model answer

    Waves cut a notch at the base of a rock face between the tide marks. The overhang collapses, and repeated notching and collapse produce a steepening cliff.

  2. 2

    Why does a cliff retreat parallel to itself?

    Model answer

    Each cycle of notching and collapse removes a slice from the cliff foot. The face keeps its angle and moves landward rather than becoming lower.

  3. 3

    What controls the angle of a cliff profile?

    Model answer

    Rock resistance, the dip of the strata and the rate of sub-aerial weathering set the angle. Strong, landward-dipping rock gives a near vertical face.

  4. 4

    Explain the formation of a wave-cut platform.

    Model answer

    As the cliff retreats it leaves behind the base of the notch as a gently sloping rock bench. Abrasion by sediment dragged across the surface smooths and lowers the platform.

  5. 5

    What is the typical gradient of a wave-cut platform?

    Model answer

    A wave-cut platform typically slopes seaward at less than 4°. The gentle angle keeps the platform within the intertidal zone.

  6. 6

    Why does a wave-cut platform limit its own growth?

    Model answer

    A wide platform makes waves break further offshore and lose energy crossing it. Less energy reaches the cliff, so retreat slows and the platform stops widening.

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