earthquakes by mr. d and some slides taken from the usgs

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Earthquakes By Mr. D and some slides taken from the USGS

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Page 1: Earthquakes By Mr. D and some slides taken from the USGS

Earthquakes By Mr. D and some slides taken from the USGS

Page 2: Earthquakes By Mr. D and some slides taken from the USGS

Earthquakes usually occur on faults caused by the subduction of two plates

Page 3: Earthquakes By Mr. D and some slides taken from the USGS

Lisa WaldUSGS Pasadena

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

USGS Earthquake Hazards Program

Plate Tectonics

Page 4: Earthquakes By Mr. D and some slides taken from the USGS

Plate Boundaries

Page 5: Earthquakes By Mr. D and some slides taken from the USGS

Three Types of Faults

Strike-SlipThrust

Normal

Page 6: Earthquakes By Mr. D and some slides taken from the USGS

Strike-slip Fault Example

Page 7: Earthquakes By Mr. D and some slides taken from the USGS

Normal Fault Example

Dixie Valley-Fairview Peaks, Nevada earthquakeDecember 16, 1954

Page 8: Earthquakes By Mr. D and some slides taken from the USGS

Thrust Fault Example

Page 9: Earthquakes By Mr. D and some slides taken from the USGS

Thrust Fault Example

Page 10: Earthquakes By Mr. D and some slides taken from the USGS

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

Page 11: Earthquakes By Mr. D and some slides taken from the USGS

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

Page 12: Earthquakes By Mr. D and some slides taken from the USGS

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

Page 13: Earthquakes By Mr. D and some slides taken from the USGS

Is there such a thing as “Earthquake Weather”???

Page 14: Earthquakes By Mr. D and some slides taken from the USGS

Earthquake Effects - Ground Shaking

Northridge, CA 1994

Page 15: Earthquakes By Mr. D and some slides taken from the USGS

Earthquake Effects - Ground Shaking

KGO-TV News ABC-7

Loma Prieta, CA 1989

Page 16: Earthquakes By Mr. D and some slides taken from the USGS

Earthquake Effects - Surface Faulting

Landers, CA 1992

Page 17: Earthquakes By Mr. D and some slides taken from the USGS

Earthquake Effects - Landslides

Turnagain Heights, Alaska,1964 (upper left inset);Santa Cruz Mtns, California , 1989

Source: National Geophysical Data Center

Page 18: Earthquakes By Mr. D and some slides taken from the USGS

Earthquake Effects - Fires

KGO-TV News ABC-7

Loma Prieta, CA 1989

Page 19: Earthquakes By Mr. D and some slides taken from the USGS

Earthquake Effects - Tsunamis

Photograph Credit: Henry Helbush. Source: National Geophysical Data Center

2011 Tsunami in Japan

Page 20: Earthquakes By Mr. D and some slides taken from the USGS

Seismic Waves

Page 21: Earthquakes By Mr. D and some slides taken from the USGS

Richter magnitude scale

• One way we measure magnitude.

• Developed in 1935 by Charles Richter in partnership with Beno Gutenberg, both of the California Institute of Technology.

• An earthquake that measures 5.0 on the Richter scale has a shaking amplitude 10 times larger than one that measures 4.0.

Page 22: Earthquakes By Mr. D and some slides taken from the USGS

Earthquake Magnitude

Page 23: Earthquakes By Mr. D and some slides taken from the USGS

Earthquake Magnitude ScaleMagnitude Earthquake Effects Estimated

• 2.5 or less: Usually not felt, but can be recorded by seismograph (frequently occurs in CA).

• 2.5 to 5.4: Often felt, but only causes minor damage. • 5.5 to 6.0: Slight damage to buildings and other structures.• 6.1 to 6.9May cause a lot of damage in very populated

areas.• 7.0 to 7.9: Major earthquake. Serious damage.20• 8.0 or greater: Great earthquake. Can totally destroy

communities near the epicenter.

Page 24: Earthquakes By Mr. D and some slides taken from the USGS

EPICENTER

• the point on the Earth's surface that is directly above the hypocenter or focus, the point where an earthquake or underground explosion originates.

Page 26: Earthquakes By Mr. D and some slides taken from the USGS

The San Andreas Fault

Page 27: Earthquakes By Mr. D and some slides taken from the USGS

Pacific-North American Plate Boundary

Page 28: Earthquakes By Mr. D and some slides taken from the USGS

Will California eventually fall into the ocean???

Page 29: Earthquakes By Mr. D and some slides taken from the USGS

Why not?

• The motion between the pacific and the north American plates beneath us is mostly horizontal. That is, the Pacific plate is moving "up" the coast, not away from the North American plate, at a rate of dozens of millimeters per year.

• So in several million years, residents of San Francisco will see the L.A. skyline out their windows.

Page 30: Earthquakes By Mr. D and some slides taken from the USGS

Faultsof SouthernCalifornia

Source: SCEC Data Center

Page 31: Earthquakes By Mr. D and some slides taken from the USGS

Shaking Hazard in Southern California

Page 32: Earthquakes By Mr. D and some slides taken from the USGS

Real-time Earthquake Information

Page 33: Earthquakes By Mr. D and some slides taken from the USGS

Any Questions?

• Remember you will have a test on this- so ask the questions now before you forget.