Slide 10
Seismic wave behavior
P waves arrive first, then S waves, then L and R
Average speeds for all these waves is known
After an earthquake, the difference in arrival times at a seismograph station can be used to calculate the distance from the seismograph to the epicenter.
Slide 11
How is an Earthquake’s Epicenter Located?
Time-distance graph showing the average travel times for P- and S-waves. The farther away a seismograph is from the focus of an earthquake, the longer the interval between the arrivals of the P- and S- waves
Slide 12
How is an Earthquake’s Epicenter Located?
Three seismograph stations are needed to locate the epicenter of an earthquake
A circle where the radius equals the distance to the epicenter is drawn
The intersection of the circles locates the epicenter
Slide 13
Modified Mercalli Intensity Map
1994 Northridge, CA earthquake, magnitude 6.7
Intensity
subjective measure of the kind of damage done and people’s reactions to it
isoseismal lines identify areas of equal intensity
Slide 14
How are the Size and Strength of an Earthquake Measured?
Magnitude
Richter scale measures total amount of energy released by an earthquake; independent of intensity
Amplitude of the largest wave produced by an event is corrected for distance and assigned a value on an open-ended logarithic scale
Slide 15
Ground Shaking
amplitude, duration, and damage increases in poorly consolidated rocks
Slide 16
Earthquake Precursors
changes in elevation or tilting of land surface, fluctuations in groundwater levels, magnetic field, electrical resistance of the ground
seismic dilatancy model
seismic gaps
Slide 17
Can Earthquakes be Predicted?
Earthquake Prediction Programs
include laboratory and field studies of rocks before, during, and after earthquakes
monitor activity along major faults
produce risk assessments
Slide 18