Hazards 4 Seismic Hazards

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Nature and Distribution:

  • Earthquake: as the crust of Earth is constantly moving, there tends to be a slow build up of stress within the rocks. When this pressure is released, parts of the surface experience, for a short period, an intense shaking motion. This is an earthquake.
  • Focus: the point at which the pressure is released in the crust
  • Epicentre: the point immediately above the focus on the Earths surface
  • Constructive plate margins:
    • Shallow focus
    • Often occur at mid ocean ridges so pose no threat to humans
  • Collision plate margins (continental/continental)
    • Shallow focus
    • Form fold mountains
  • Conservative plate margins:
    • Shallow focus
  • Destructive plate boundaries:
    • Deep foci
    • Occur in the Benioff zone (where oceanic crust is being subducted under the continental crust)
  • 90% of earthquakes are at plate boundaries, 10% are intraplate
  • In 2002 in the UK Midlands a 4.8 EQ occurred, which was caused by movements on an old fault line
  • seismometer: the instrument that measures the seismic waves generated by an earthquake

Magnitude and Frequency:

  • Richter Scale:
    • The amplitude of the largest recorded seismic wave and the distance between the focus and the seismometer 
    • A 1-10 scale
    • Not accurate when measuring large scale earthquakes
  • Moment Magnitude Scale:
    • The total moment released of the EQ, where a moment is the product of the distance the fault  has moved and the force required to move it
    • A 1-10 scale
    • Used globally
    • Up to 8, very similar to Richter scale, but above it, it is more accurate
  • Mercalli Scale:
    • Uses observations of people to determine the amount of damage caused by the event
    • A 12 point scale
  • The UK experiences 20-30 earthquakes per year

Primary Effects:

  • Body waves:
    • P waves:
      • Travel through liquids and solids
      • Travel at 5.5km/s
      • Faster than S waves
    • S waves:
      • Travel through solids
      • Travel at 3km/s
      • Slower than P waves
  • Surface waves:
    • Love waves:
      • Shake the ground at right angles to the direction of movement
    • Rayleigh waves:
      • Have a rolling motion

Secondary Effects:

  • Liquefaction
    • Soils with high water content lose their mechanical strength and start to behave as a liquid
  • Landslides/avalanches
  • Tsunamis
  • Fires
    • As a result from broken gas pipes and collapsed electricity transmission services
  • Effects on people and the built environment
    • Collapsing buildings, destruction of road systems, destruction of communication systems, destruction of service provisions: water, electricity, gas, flooding, food shortages, disruption to the local economy

Short Term Impacts:

  • 3/4 deaths are from falling buildings
  • Rapid urbanisation has increased the earthquake risk. Low cost and poorly built housing make people is slums disproportionately vulnerable 
  • The destruction of infrastructure will hinder the rescue efforts 
  • Contamination of the water supply

Long Term Impacts

  • The effect on the economy

Prediction:

  • Prediction is very difficult
  • Monitoring groundwater levels, release of radon gas, unusual animal behaviour
  • Fault lines can be monitored and local magnetic fields measured
  • A study of the San Andreas fault between 1969

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