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4. HOW THE GROUND SHAKES What happened in past quakes & will happen in future ones
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4. HOW THE GROUND SHAKES What happened in past quakes & will happen in future ones.

Dec 22, 2015

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Page 1: 4. HOW THE GROUND SHAKES What happened in past quakes & will happen in future ones.

4. HOW THE GROUND SHAKES

What happened in past quakes & will happen in future ones

Page 2: 4. HOW THE GROUND SHAKES What happened in past quakes & will happen in future ones.

Disturbances as function of space & time that travel through solid earth

Like electromagnetic (light) waves, water waves, or sound (ultrasound, sonar, dolphins, bats)

Use to study earthquakes and “see” earth structure

Davidson 8.11

SEISMIC WAVES

Page 3: 4. HOW THE GROUND SHAKES What happened in past quakes & will happen in future ones.

Seismic waves occur because an applied force

makes rock deform elastically & then return to

original shape

Compression - volume changes

Shear distortion: shape changes

Davidson 5.3

Page 4: 4. HOW THE GROUND SHAKES What happened in past quakes & will happen in future ones.

P or compressional waves - volume changes - material compressed or expanded in direction wave propagates

S or shear waves - distortion without volume changes - material sheared in direction perpendicular to wave propagation

DD 7.2

Page 5: 4. HOW THE GROUND SHAKES What happened in past quakes & will happen in future ones.

DD 7.5

April 18, 2008 09:37Southern Illinois M 5.4

3 component seismograms

Earthscope transportable array at Hobbs, NM

P wave travel time (min)

Page 6: 4. HOW THE GROUND SHAKES What happened in past quakes & will happen in future ones.

P wave travel time (min)

Activity 4.1:

How fast in miles per hour do seismic waves travel?

Page 7: 4. HOW THE GROUND SHAKES What happened in past quakes & will happen in future ones.

Seismic wave amplitudes

decrease with distance from an earthquake

DD 7.7Hough et al 2000

University of Nevada, Reno

Shaking and damage decrease

with distance

Page 8: 4. HOW THE GROUND SHAKES What happened in past quakes & will happen in future ones.

Seismic waves travel better in the colder rock of the stable Midwest than in the west

An earthquake in the Midwest causes more shaking than a similar sized one in the west

S. HoughDD 7.8

Page 9: 4. HOW THE GROUND SHAKES What happened in past quakes & will happen in future ones.

Seismic wave amplitudes increase as waves travel from solid (faster) rock to weaker (slower) material, so buildings on soft sediment are more vulnerable than ones on solid rock DD 7.10

San Francisco Marina district landfill

1989 Loma Prieta earthquake

Page 10: 4. HOW THE GROUND SHAKES What happened in past quakes & will happen in future ones.

This is analogous to the way water waves grow taller as they go from deep to shallow water

DD 7.10

2004 Sumatra earthquake tsunami

Page 11: 4. HOW THE GROUND SHAKES What happened in past quakes & will happen in future ones.

Arrival times of seismic waves used to locate earthquakes

Amplitudes used to find magnitudes

DD 8.9

Page 12: 4. HOW THE GROUND SHAKES What happened in past quakes & will happen in future ones.

Pattern of seismic waves radiated by earthquakes used to find fault geometry & dimensions

DD 8.9

Page 13: 4. HOW THE GROUND SHAKES What happened in past quakes & will happen in future ones.

At interfaces, seismic waves change direction and amplitude

DD 7.11

These changes reveal the physical properties within the earth

Page 14: 4. HOW THE GROUND SHAKES What happened in past quakes & will happen in future ones.

Analyzing the times and amplitudes of seismic waves is the primary tool for studying structure of

the earth

Stein & Wysession, 2003