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Earthquakes Photo credit: USGS
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Causes of Earthquakes Types and Behavior of Seismic Waves Body Waves
Primary or Compressional Secondary or Shear Surface Waves Raleigh (large vertical displacements) Love (shear)
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Elastic Rebound Theory
3 m offset 1906 San Francisco Earthquake
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Elastic Rebound Animation
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Offset Lettuce Rows - El Centro, CA
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Earthquake Focus and Hypocenter
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Earthquake Focus Animation
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Seismic Wave Types Body Waves Surface Waves
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equations for velocities
Vp = k + 4/3µ r 1/2 r density shear modulus (rigidity) Vs = µ r k bulk modulus (rigidity) 1/2 because shear modulus (rigidity) for fluid is zero, S waves cannot propagate through a fluid consequence of equations is that P waves are 1.7x faster than S can infer physical properties from P and S waves
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Wave Animations
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Locating and Measuring Earthquakes
Determining the Location of an Earthquake Measuring the Size of an Earthquake Location and Size of Earthquakes in the United States
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Vertical Component Seismometer
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Horizontal Component Seismomter
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Seismograph Animation
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First Arrivals - Seismographic Records
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Distance - Time Relations
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P vs. S Wave Travel Time Curves
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Earthquake Location by Range
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Effects of Earthquakes
Tsunamis World Distribution of Earthquakes First-Motion Studies of Earthquakes
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Modified Mercalli Intensity Index (1931)
1886 Charleston, SC earthquake
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Pancaked Building - 1985 Mexico City
Earthquakes don’t kill people - buildings do!
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