Earthquakes 101 (EQ101)

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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)

description

Earthquakes 101 (EQ101). USGS Earthquake Hazards Program. Lisa Wald USGS Pasadena. U.S. Department of the Interior U.S. Geological Survey. Global Distribution of Earthquakes. Plate Tectonics. USGS Earthquake Hazards Program. Lisa Wald USGS Pasadena. U.S. Department of the Interior - PowerPoint PPT Presentation

Transcript of Earthquakes 101 (EQ101)

Page 1: Earthquakes 101 (EQ101)

Lisa WaldUSGS Pasadena

U.S. Department of the InteriorU.S. Geological Survey

USGS Earthquake Hazards Program

Earthquakes 101 (EQ101)

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Global Distribution of Earthquakes

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Lisa WaldUSGS Pasadena

U.S. Department of the InteriorU.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-SlipThrust

Normal

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Normal Fault Example

Dixie Valley-Fairview Peaks, Nevada earthquakeDecember 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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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 EarthquakeTotal 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 EarthquakesBigger Faults Make Bigger Earthquakes

1

10

100

1000

5.5 6 6.5 7 7.5Magnitude

Kilo

me

ters

8

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Bigger Earthquakes Last a Longer TimeBigger Earthquakes Last a Longer Time

1

10

100

5.5 6 6.5 7 7.5 8

Magnitude

Sec

onds

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What Controls the Level of Shaking?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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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

55 KM longLast ruptured in last 10,000 YEARSSLIP 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 longLast ruptured in last 10,000 YEARSSLIP RATE: between 0.10 and 0.22 mm/yr

PROBABLE MAGNITUDES: MW6.0 - 7.0Dips 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

18 KM longLast ruptured in last 1.6 million YEARSSLIP 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?

CommunityInternetIntensityMaps

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U.S. Department of the InteriorU.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 faultSlip on an earthquake fault

START

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Slip on an earthquake faultSecond 2.0Slip on an earthquake faultSecond 2.0

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Slip on an earthquake faultSecond 4.0Slip on an earthquake faultSecond 4.0

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Slip on an earthquake faultSecond 6.0Slip on an earthquake faultSecond 6.0

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Slip on an earthquake faultSecond 8.0Slip on an earthquake faultSecond 8.0

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Slip on an earthquake faultSecond 10.0Slip on an earthquake faultSecond 10.0

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Slip on an earthquake faultSecond 12.0Slip on an earthquake faultSecond 12.0

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Slip on an earthquake faultSecond 14.0Slip on an earthquake faultSecond 14.0

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Slip on an earthquake faultSecond 16.0Slip on an earthquake faultSecond 16.0

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Slip on an earthquake faultSecond 18.0Slip on an earthquake faultSecond 18.0

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Slip on an earthquake faultSecond 20.0Slip on an earthquake faultSecond 20.0

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Slip on an earthquake faultSecond 22.0Slip on an earthquake faultSecond 22.0

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Slip on an earthquake faultSecond 24.0Slip on an earthquake faultSecond 24.0