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Hazardous Earth

Tsunamis from sea-bed uplift and underwater landslides

  • 2 things to know
  • Component 03

Overview

Recall questions on how subduction earthquakes and underwater landslides generate tsunamis, why strike-slip faults rarely do, open-ocean wavelength and speed with a worked calculation, shoaling, run-up and drawback, successive waves, the 2004 Indian Ocean and 2011 Japanese tsunamis, sea-bed pressure sensors, and warning times.

What you need to know

Answer each one before you reveal it.

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Key term

Why is the first tsunami wave often not the most dangerous?

Key term

Define a tsunami.

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Define a tsunami.

    Model answer

    A series of very long waves generated by the sudden displacement of a large volume of sea water.

  2. 2

    How does a subduction earthquake generate a tsunami?

    Model answer

    The overriding plate, held down by friction, snaps upwards when the fault ruptures and lifts the whole column of water above it, which then spreads outwards as waves.

  3. 3

    Why does a strike-slip earthquake rarely cause a tsunami?

    Model answer

    Its movement is horizontal, so it displaces almost no water vertically.

  4. 4

    State the typical wavelength of a tsunami in the open ocean.

    Model answer

    Between about 100 and 200 km.

  5. 5

    Why is a tsunami almost undetectable to a ship in deep water?

    Model answer

    Its height is less than a metre and its wavelength is so long that the sea surface rises and falls too gradually for anyone on board to notice.

  6. 6

    A tsunami crosses ocean 4,000 m deep. Given that its speed equals the square root of gravitational acceleration multiplied by water depth, calculate that speed.

    Model answer

    The speed is √(9.81 × 4,000) = √39,240, which is about 198 m s⁻¹, or roughly 710 km per hour.

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