Earth's Internal Structure: Seismic Waves (2.2.3) Flashcards

1
Q

Energy and Seismic Waves

A
  • Measure energy in joules (1 J = 1 Nm).
  • Seismic waves emanate out all directions from earthquake focus.
  • Surface waves: analogous to water waves, travel along Earth’s surface.
  • Body waves: travel through interior (faster than surface waves).
  • P-wave (pressure wave)
  • S-wave (shear wave)
  • Rayleigh wave
  • Love wave
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2
Q

How is magnitude of earthquakes measured?

A
  • Use Moment Magnitude Scale (not Richter Scale).
  • Based on energy released (area of rupture x slip x rock rigidity).
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3
Q

How often do large earthquakes occur?

A
  • Only 7 large earthquakes (>8.8 magnitude) have occurred since 1900.
  • 3 of them occurred past 15 years.
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4
Q

How are historical earthquake sizes estimated?

A
  • Moment Magnitude Scale and Richter Scale can’t be applied to any pre-WWII.
  • Modified Mercalli Scale used (qualitative scale based on effects of earthquake from I to XII).
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5
Q

What are the travel and arrival times of seismic waves?

A
  • Body waves travel shorter distances than surface waves.
  • Body waves faster than surface waves.
  • P-, S-waves arrive first, followed by Love, Rayleigh waves.
  • Difference in arrival times of P- and S-waves = locate epicentre of earthquake.
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