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Coastal Landscapes

Emergent coasts: raised beaches, marine terraces and abandoned cliffs

  • 2 things to know
  • Component 01

Overview

Recall questions on emergent coastlines, eustatic and isostatic change in sea level, the last glacial maximum and isostatic rebound, why raised beaches are common in Scotland, marine terraces, abandoned cliffs and their features, and how present-day sea level rise could change them.

What you need to know

Answer each one before you reveal it.

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Key term

What is an emergent coastline?

Key term

Explain how a cooling climate lowers sea level.

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What is an emergent coastline?

    Model answer

    A coast where the land now stands higher relative to the sea than it did in the past, so former marine landforms are exposed above the present shore.

  2. 2

    Explain how a cooling climate lowers sea level.

    Model answer

    Water evaporated from the oceans is locked up in growing ice sheets and glaciers instead of returning as runoff, so the volume of water in the oceans falls.

  3. 3

    What is a eustatic change in sea level?

    Model answer

    A worldwide change in the volume of water held in the oceans, and therefore a change in sea level everywhere.

  4. 4

    What is an isostatic change in sea level?

    Model answer

    A local change in the level of the land itself, such as the crust sinking under the weight of an ice sheet or rising again once the ice has melted.

  5. 5

    By roughly how much did global sea level fall at the height of the last glacial period?

    Model answer

    By about 120 metres below its present level.

  6. 6

    When did the last glacial maximum occur?

    Model answer

    About 20,000 years ago.

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AThe lower quartile is the 2nd value, 11 cm.
BThe upper quartile is the 6th value, 16 cm.
CThe interquartile range is 16 − 11 = 5 cm.

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