Active Deformation of the San Francisco Bay Areaburgmann/EDUCATION2/Bay_area_def.… · 2.5 ± 3.9...
Transcript of Active Deformation of the San Francisco Bay Areaburgmann/EDUCATION2/Bay_area_def.… · 2.5 ± 3.9...
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Active Deformation of the SanFrancisco Bay Area
• The Cause: Plate tectonics in California
• The Culprit: The San Andreas fault system
• The Consequences: Earthquakes and theearthquake cycle along the San Andreas
• The Connection: Earthquakes and landscapes as aresult of deformation along the San Andreas fault
• The “Cure”: Understanding, forecasting and livingwith earthquakes in the Bay area
BASP Lecture - 08/13/2001 available @: www.seismo.berkeley.edu/~burgmann/education.html
Fundamental Questions• “Is California going to fall in the ocean?” or
“What is the long-term tectonic development of the SanAndreas fault system?”
Plate Tectonics
Bay AreaFuture
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GeometryFault
Kinematics
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Preparedness
Earthquake Hazard
EarthquakeHistory
DeformationMeasurements
Fundamental Questions• “When is the next Big One?” or
“Can we predict earthquakes based on our understanding ofthe history and mechanics of San Andreas faulting”?
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The Cause: Plate Tectonics• Evolution of the Pacific - North
America plate boundary
Press and Sievers, 2001
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At the Root of it All: Plate Tectonics• Evolution of the Pacific -
North America PlateBoundary
• The San Andreas faultsystem
Tanya Atwater, UCSB
The Culprit: The San AndreasFault System
• Where are the faultsand how do theymove?
• Plate tectonicspredicts lateral motionbetween Pacific andNorth American plates
• Faults that movelaterally (rather thanup and down) arecalled strike-slip faults
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Strike-slip Faults
• No shortening
• No uplift
The San Andreas fault is a right-lateral fault
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Strike-slip Faults
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Right-lateral Hayward Fault
The SAF System in the Bay Area• Where is
deformationtaking place inthe Bay Area?
• Look at geology,landscapes, andlocation ofearthquakes
40 mm
/yr
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Only Strike-slip Faults in Bay Area?
• Where do the hills come from?
Thrust faults in the Bay area
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The Consequences:Earthquakes
Elastic Strain Accumulation
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• Earthquakes represent the shaking associatedwith fault rupture
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The Earthquake Cycle
Demonstrating the EarthquakeCycle
• You can producesteady sliding(creep) and stick slip(earthquakes) in asimple table topexperiment
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Earthquakes vs. Fault Creep
Downtown Hayward, 1868
http://www.seismo.berkeley.edu/seismo/geotour/stadium.html
Current Seismicity Informationat Your Finger Tips
quake.wr.usgs.gov/QUAKES/CURRENT/index.htmlwww.seismo.berkeley.edu/seismo/
neic.usgs.gov/neis/current/
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The Connection: Earthquakes andthe Bay Area
• The hills, the valleys, the Bay, the soils, the climate,flora, and fauna are all linked to earthquakes shapingthe earth through geologic time
Why Study Earthquakes?
• Evidence of plate tectonics and the evolution ofgeology and landscapes
• Earthquake hazard and mitigation
• Earthquake forecasting and prediction
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The “Cure”: UnderstandingEarthquakes in Bay Area
Bay Area Earthquake History
• 16 M > 6 Quakes in 80years before 1906
• 5 M > 6 Quakes in 95years after 1906
• Good or bad news?
USGS
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Living in an Earthquake’s Shadow
• San Andreas F.– 1906 Mw=7.7– Ruptured from
San JuanBautista to CapeMendocino
– Relieved largeamount of stress
– Is the springloaded again?
40 mm
/yr
Dating Earthquake Fossils:Paleoseismology
• Digging up faults• Date earthquakes using 14C
Extend earthquake recordback 1000s of years
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BRIB
San Andreas fault�
Hayward fault�
Calaveras fault�
Greenville fault�
Fremont�Berkeley �
Pt. Pinole�Pt. Pinole�Pt. Pinole�
20 mm/yr
2.5 ± 3.9 mm/yr
17.1 ± 5.1 mm/yr
9.9 ± 2.5 mm/yr
22.7 ± 1.7 mm/yr
Geodesy Measures ActiveStrain Accumulation
• GPS allows us tomeasure strainaccumulation
• We can determinefault slip rates
Forecasting Earthquakes
• We can not predictearthquakes.
• Using historic and pre-historic earthquake patterns,fault slip rates, and geodeticmeasurements we canestimate probability of futureearthquakes
quake.wr.usgs.gov/research/seismology/wg99/index.html
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Earthquake Hazard Factors• The substrate
matters!
• Stable bedrockgood
• mud and fillbad
USGS
Shaking Hazard Maps
www.abag.ca.gov/bayarea/eqmaps/eqmaps.html
S Hayward fault earthquake
San Andreas (1906-type) earthquake
• Shaking hazard &damage depend on:
– Earthquake magnitude– Distance to earthquake– Quality of construction
– Soil properties
•You can view shakingintensities from many scenarioearthquakes for all cities on theweb.• Of course, quality ofconstruction is as important