Earthquakes 101 (EQ101)

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Earthquakes 101 (EQ101)
USGS Earthquake Hazards Program
Lisa Wald USGS Pasadena
U.S. Department of the Interior U.S. Geological
Survey
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Global Distribution of Earthquakes
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Plate Tectonics
USGS Earthquake Hazards Program
Lisa Wald USGS Pasadena
U.S. Department of the Interior U.S. Geological
Survey
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Plate Boundaries
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Watch southern california video
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Three Types of Faults
Strike-Slip
Thrust
Normal
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Normal Fault Example
Dixie Valley-Fairview Peaks, Nevada
earthquake December 16, 1954
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Thrust Fault Example
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Thrust Fault Example
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Strike-slip Fault Example
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Strike-slip Fault Example
1906 San Francisco Earthquake
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Strike-slip Fault Example
Landers, CA 1992
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Where is Haiti?
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Total Slip in the M7.3 Landers Earthquake
Rupture on a Fault
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Seismic Waves
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Earthquake Magnitude
M5
M6
M7
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Earthquake Location
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Bigger Faults Make Bigger Earthquakes
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Bigger Earthquakes Last a Longer Time
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What Controls the Level of Shaking?

• Magnitude
• More energy released
• Distance
• Shaking decays with distance
• Local soils
• amplify the shaking

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Is there such a thing as Earthquake Weather???
No!
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Earthquake Effects - Ground Shaking
Northridge, CA 1994
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Earthquake Effects -Ground Shaking
Northridge, CA 1994
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Earthquake Effects - Ground Shaking
Loma Prieta, CA 1989
KGO-TV News ABC-7
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Earthquake Effects - Ground Shaking
Kobe, Japan 1995
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Earthquake Effects - Ground Shaking
Kobe, Japan 1995
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Earthquake Effects - Surface Faulting
Landers, CA 1992
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Earthquake Effects - Liquefaction
Source National Geophysical Data Center
Niigata, Japan 1964
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Earthquake Effects - Landslides
Source National Geophysical Data Center
Turnagain Heights, Alaska,1964 (upper left
inset) Santa Cruz Mtns, California , 1989
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Earthquake Effects - Fires
Loma Prieta, CA 1989
KGO-TV News ABC-7
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Earthquake Effects - Tsunamis
1957 Aleutian Tsunami
Photograph Credit Henry Helbush. Source
National Geophysical Data Center
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The San Andreas Fault
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Pacific-North American Plate Boundary
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Will California eventually fall into the ocean???
No!
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Faultsof SouthernCalifornia
Source SCEC Data Center
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Shaking Hazard in Southern California
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Faults in Our Local Area - Arcadia

Sierra Madre Fault Zone
THRUST fault
55 KM long
Last ruptured in last 10,000 YEARS
SLIP RATE between 0.36 and 4 mm/yr
PROBABLE MAGNITUDES MW6.0 - 7.0 (?) Dips to the
north
Source SCEC Data Center
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Faults in Our Local Area - Arcadia

Raymond Fault
STRIKE-SLIP fault
26 KM long
Last ruptured in last 10,000 YEARS
SLIP RATE between 0.10 and 0.22 mm/yr
PROBABLE MAGNITUDES MW6.0 - 7.0 Dips to the north
Source SCEC Data Center
At least eight surface-rupturing events have
occurred along this fault in the last 36,000 years
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Faults in Our Local Area - Arcadia

Clamshell-Sawpit Canyon fault
THRUST fault
18 KM long
Last ruptured in last 1.6 million YEARS
SLIP RATE ???
PROBABLE MAGNITUDES ??? Dips to the north
Source SCEC Data Center
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Real-time Earthquake Information
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ShakeMaps
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Did You Feel It?
Community Internet Intensity Maps
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USGS Earthquake Hazards Program
U.S. Department of the Interior U.S. Geological
Survey
Where to go for more information
http//pasadena.wr.usgs.gov/ http//earthquake.usg
s.gov/
The End
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Faults in Our Local Area - La Canada

TYPE OF FAULTING reverse
LENGTH the zone is about 55 km long total
length of main fault segments is about 75
km, with each segment measuring roughly 15 km long
MOST RECENT SURFACE RUPTURE Holocene, 10,000
years to present
SLIP RATE between 0.36 and 4 mm/yr
INTERVAL BETWEEN SURFACE RUPTURES several
thousand years (?)
PROBABLE MAGNITUDES MW6.0 - 7.0 (?) OTHER
NOTES This fault zone dips to the north.
Source SCEC Data Center
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Slip on an earthquake fault
Surface of the earth
Depth Into the earth
100 km (60 miles)
Distance along the fault plane
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Slip on an earthquake faultSecond 2.0
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Slip on an earthquake faultSecond 4.0
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Slip on an earthquake faultSecond 6.0
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Slip on an earthquake faultSecond 8.0
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Slip on an earthquake faultSecond 10.0
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Slip on an earthquake faultSecond 12.0
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Slip on an earthquake faultSecond 14.0
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Slip on an earthquake faultSecond 16.0
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Slip on an earthquake faultSecond 18.0
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Slip on an earthquake faultSecond 20.0
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Slip on an earthquake faultSecond 22.0
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Slip on an earthquake faultSecond 24.0