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)
Elastic Rebound Theory 3 m offset 1906 San Francisco Earthquake
Elastic Rebound Animation
Offset Lettuce Rows - El Centro, CA
Earthquake Focus and Hypocenter
Earthquake Focus Animation
Seismic Wave Types Body Waves Surface Waves
equations for velocities Vp = Vs = k + 4/3µ r 1/2 r density µ shear modulus (rigidity) k bulk modulus (rigidity) because shear modulus (rigidity) for fluid is zero, S waves cannot propagate through a fluid consequence of equations is that P waves are 1. 7 x faster than S can infer physical properties from P and S waves
Wave Animations
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
Vertical Component Seismometer
Horizontal Component Seismomter
Seismograph Animation
First Arrivals - Seismographic Records
Distance - Time Relations
P vs. S Wave Travel Time Curves
Earthquake Location by Range
Effects of Earthquakes • Tsunamis • World Distribution of Earthquakes • First-Motion Studies of Earthquakes
Modified Mercalli Intensity Index (1931) 1886 Charleston, SC earthquake
Pancaked Building - 1985 Mexico City Earthquakes don’t kill people - buildings do!