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Lisa Wald USGS Pasadena U.S. Department of the Interior U.S. Geological Survey USGS Earthquake Hazards Program Earthquakes 101 (EQ101)
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Global Distribution of Earthquakes
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Lisa Wald USGS Pasadena U.S. Department of the Interior U.S. Geological Survey USGS Earthquake Hazards Program Plate Tectonics
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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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Strike-slip Fault Example
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1906 San Francisco Earthquake
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Landers, CA 1992 Strike-slip Fault Example
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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”???
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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 KGO-TV News ABC-7 Loma Prieta, CA 1989
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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 Turnagain Heights, Alaska,1964 (upper left inset); Santa Cruz Mtns, California, 1989 Source: National Geophysical Data Center
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Earthquake Effects - Fires KGO-TV News ABC-7 Loma Prieta, CA 1989
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Earthquake Effects - Tsunamis Photograph Credit: Henry Helbush. Source: National Geophysical Data Center 1957 Aleutian Tsunami
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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???
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Faults of Southern California Source: SCEC Data Center
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Shaking Hazard in Southern California
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Faults in Our Local Area - Arcadia Source: SCEC Data Center 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 THRUST fault Sierra Madre Fault Zone
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Faults in Our Local Area - Arcadia Source: SCEC Data Center 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 STRIKE-SLIP fault Raymond Fault 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 Source: SCEC Data Center 18 KM long Last ruptured in last 1.6 million YEARS SLIP RATE: ??? PROBABLE MAGNITUDES: ??? Dips to the north THRUST fault Clamshell-Sawpit Canyon fault
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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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U.S. Department of the Interior U.S. Geological Survey USGS Earthquake Hazards Program http://pasadena.wr.usgs.gov/ http://earthquake.usgs.gov/ Where to go for more information:
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Faults in Our Local Area - La Canada Source: SCEC Data Center 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. TYPE OF FAULTING: reverse
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Depth Into the earth Surface of the earth Distance along the fault plane 100 km (60 miles) Slip on an earthquake fault START
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Slip on an earthquake fault Second 2.0
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Slip on an earthquake fault Second 4.0
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Slip on an earthquake fault Second 6.0
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Slip on an earthquake fault Second 8.0
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Slip on an earthquake fault Second 10.0
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Slip on an earthquake fault Second 12.0
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Slip on an earthquake fault Second 14.0
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Slip on an earthquake fault Second 16.0
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Slip on an earthquake fault Second 18.0
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Slip on an earthquake fault Second 20.0
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Slip on an earthquake fault Second 22.0
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Slip on an earthquake fault Second 24.0
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