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Earthquake Hazard: Ground Shaking

Ground Shaking

  • ground shakes

  • buildings and things inside may fall

  • 1556 Shaanxi province, china

    • worst recorded earthquake for fatalities

    • housing was silt (very fine-grained sediment) caves, most collapsed

    • 883,000 people died

  • buildings on solid rock or compacted sediments are safer

  • wet, loose sediment and artificial fill have longer and more intense shaking

    • also prone to liquefaction

  • shaking can trigger resonance in a building

    • amplitude of the wave increases when the frequency of the seismic wave is the same or very close to the natural frequency of the building

  • hypocenter: point on the fault where motion starts

  • epicenter: directly above hypocenter on surface

  • when the ground shakes, it creates a fault scarp

    • fault scarp: exposure of the fault visible at the surface; exposed due to offset (movement) along the fault

  • elastic rebound theory: explains how energy builds up and is then released in an earthquake and how that energy is released

    • this can create ground shaking

AS

Earthquake Hazard: Ground Shaking

Ground Shaking

  • ground shakes

  • buildings and things inside may fall

  • 1556 Shaanxi province, china

    • worst recorded earthquake for fatalities

    • housing was silt (very fine-grained sediment) caves, most collapsed

    • 883,000 people died

  • buildings on solid rock or compacted sediments are safer

  • wet, loose sediment and artificial fill have longer and more intense shaking

    • also prone to liquefaction

  • shaking can trigger resonance in a building

    • amplitude of the wave increases when the frequency of the seismic wave is the same or very close to the natural frequency of the building

  • hypocenter: point on the fault where motion starts

  • epicenter: directly above hypocenter on surface

  • when the ground shakes, it creates a fault scarp

    • fault scarp: exposure of the fault visible at the surface; exposed due to offset (movement) along the fault

  • elastic rebound theory: explains how energy builds up and is then released in an earthquake and how that energy is released

    • this can create ground shaking