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Hazardous Earth

Ground shaking, ground displacement and liquefaction

  • 2 things to know
  • Component 03

Overview

Recall questions on ground shaking as the primary hazard, peak ground acceleration, duration and resonance, amplification on soft ground in Mexico City in 1985, ground displacement and infrastructure, the mechanism and conditions of liquefaction, its effects on buildings, sand boils, and Christchurch in 2011.

What you need to know

Answer each one before you reveal it.

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Key term

Which three characteristics of the shaking determine how much damage a building suffers?

Key term

What is peak ground acceleration?

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Why is ground shaking considered the primary hazard of an earthquake?

    Model answer

    It is the direct effect of the seismic waves themselves, and it is what triggers almost every other hazard, from building collapse to landslides.

  2. 2

    Which three characteristics of the shaking determine how much damage a building suffers?

    Model answer

    The peak ground acceleration, the length of time the shaking lasts, and the frequency of the waves.

  3. 3

    What is peak ground acceleration?

    Model answer

    The maximum acceleration reached by the ground during an earthquake, usually expressed as a fraction of the acceleration due to gravity.

  4. 4

    Explain why the duration of shaking matters as much as its strength.

    Model answer

    Structures weakened by the first few seconds of movement are progressively broken down by every further cycle, so a long earthquake destroys buildings that would survive a short one of the same intensity.

  5. 5

    What is resonance in the context of earthquake damage?

    Model answer

    When the frequency of the ground motion matches the natural frequency of a building, the swaying is amplified with each cycle and that building suffers far worse damage than its neighbours.

  6. 6

    How does soft ground make shaking worse?

    Model answer

    Seismic waves slow down in loose sediment and their amplitude increases to carry the same energy, so unconsolidated ground shakes far more strongly than bedrock.

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