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Hazardous Earth

Earthquake focus, depth and the seismic waves released

  • 2 things to know
  • Component 03

Overview

Recall questions on the focus and epicentre, elastic rebound, stress and strain, P, S, Love and Rayleigh waves and how they move rock, the S-wave shadow zone, locating an epicentre, shallow-focus and deep-focus earthquakes and why depth matters, the 700 km limit, Benioff zones, and aftershocks.

What you need to know

Answer each one before you reveal it.

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Key term

Define the focus of an earthquake.

Key term

Define the epicentre of an earthquake.

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Define the focus of an earthquake.

    Model answer

    The point within the Earth at which the rock first ruptures and from which seismic waves begin to radiate.

  2. 2

    Define the epicentre of an earthquake.

    Model answer

    The point on the Earth's surface directly above the focus.

  3. 3

    Explain elastic rebound.

    Model answer

    Rock on either side of a locked fault deforms elastically as stress builds, and when the stress exceeds the strength of the fault the rock snaps back to its unstrained shape, releasing the stored energy as seismic waves.

  4. 4

    What is the difference between stress and strain in the crust?

    Model answer

    Stress is the force applied to the rock, while strain is the deformation the rock undergoes in response to it.

  5. 5

    Which seismic wave arrives first at a recording station, and why?

    Model answer

    The P wave, because it is the fastest, travelling roughly 1.7 times the speed of the S wave.

  6. 6

    Describe how a P wave moves the rock it passes through.

    Model answer

    It compresses and stretches the rock backwards and forwards along the direction in which the wave is travelling.

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