Name of School Date Earthquakes and Seismology. Plate Tectonics.
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Transcript of Name of School Date Earthquakes and Seismology. Plate Tectonics.
Name of School
Date
Earthquakes and Seismology
Plate Tectonics
A Century of Earthquakes: 1906-2006
Global Seismographic Network
2006 Earthquakes > M5.5
2006 Earthquakes > M5.5 in the world
How Many?
Earthquake Magnitude and Equivalent Energy Comparisons
Source: http://www.iris.edu/edu/onepagers/no3.pdf
Earthquakes generate Seismic Waves that travel around the globe and tell us about the Earth’s interior.
Simple Seismometer
A simple way to measure shaking from earthquakes.
To see it in action, watch this 14 sec videohttp://www.youtube.com/watch?v=DX5VXGmdnAg&NR=1
What is an Earthquake?
Earthquake: The sudden release of elastic energy by fracture over some area of the earth.
What is an Earthquake?
Earthquake: The sudden release of elastic energy by fracture over some area of the earth.
Earthquake: The sudden slip on a fault (release of elastic energy), and the resulting ground shaking and radiated seismic energy caused by the slip.
Fault: A fracture (crack) in the earth, where the two sides move past each other and the relative motion is parallel to the fracture.
Typical Plate Boundaries
Plate Boundaries& earthquakes
Types of Faults
A fence built over a fault…
1906 San Francisco Earthquake
Fence Offset
Offset Stream Channels in Central California
Types of Seismic Waves P-wave:
Primary Wave. Compressional wave, like a Slinky© being pushed and pulled.
S-wave: Secondary Wave. This is a shear wave where
particles move perpendicular to the travel direction of the wave.
Surface Waves: Both Love and Rayleigh Waves. Only shallow
particles are disturbed. Love waves are sideways, Rayleigh are vertical (like ocean waves).
Types of Seismic Waves
Types of Seismic Waves
Seismographs
Horizontal Vertical
Distance to quake epicenter
P
S
L
Note:P-wave firstS-wave secondSurface waves last
Time lag between p and s-wave arrival is called t.
Fig 3.22
Ts=23sTp=14s
Maximum Amplitude = 540 mm
Locating Earthquakes
Fig. 3.23
Locating Earthquakes
Locating Earthquakes
Earthquake SizeRichter Magnitude:
Relative Size of an Earthquake(based on seismograph
shaking)
Seismic Moment/Moment Magnitude: Absolute Size of an Earthquake
(based on energy released)
Modified Mercalli Intensity:How much I’m shakin’(based on talking to people)
Calculating Richter MagnitudeA.K.A Local Magnitude
ML = log10A - log10Ao
A is the amplitude of the s-wave measured at given stationAo is the amplitude of a MR=0 event at the same distance
PS
Log of the Amplitude for a Magnitude 0 Earthquake
M = 4
M = 0
Earthquake: The sudden slip on a fault (release of elastic energy), and the resulting ground shaking and radiated seismic energy caused by the slip.
Aki’s Seismic Moment Formula
Mo = s A
Where:
is the shear modulus.S is the average slip on the faulted area.A is the area of the fault plane over which slip has occurred.
Shear modulus ( can just be thought of as the strength of the faulted material
Modified Mercalli Intensity
Based on response of humans and structures
I (not felt except by few)
XII (total destruction)
Still useful for comparison with older earthquakes for which there were no instrument records
Earthquake Info on the Internet
http://earthquakes.usgs.gov/
Earthquake Info on the Internet
http://earthquakes.usgs.gov/eqcenter/dyfi.php
Did You Feel It???
Go online and tell us!
Earthquake Info on the Internethttp://www.data.scec.org/recenteqs.html
Southern California with
Faults & the Big Bend
Southern California from Space(1)
Southern California from SpaceWith a Few Major Faults
Historical Earthquakes (1800-1850)Historical Earthquakes (1850-1900)Historical Earthquakes (1900-1950)Historical Earthquakes (1950-2004)Historical Earthquakes (1000-1800)
Smith and Sandwell, 2006
Thank You for Your Attention
Questions?