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Earthquake Science (Seismology)
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Announcements for next week’s lab
Magnetometer survey, working in groups Please bring: small notebook pen graph paper umbrella (if raining) Be prepared to remove all metal (watches, belt buckles, jewelry, etc.)
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March 28, Alaska M = 9.1 Up to 12 m vertical displacement
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October 17, 1989 - Loma Prieta, CA
$6 B in property damage
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January 17, 1994 - Northridge, CA
Mw = 6.7 > $15 B in property damage
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January 17, Kobe, Japan Mw = 6.7 5000 dead, > $200 B in property damage
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August 17, Izmit, Turkey M = 7.4 15,700 casualties
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December 26, Sumatra M = 9.15 250,000 deaths
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What are earthquakes? (… and what earthquakes are not!)
Earthquake phenomenology (… fault, epicentre, seismic waves, magnitude)
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Earthquake: A sudden, violent dislocation in the subsurface caused by stress buildup on a fault.
Fence offset during the Great Earthquake (1906) 4 m San Andreas Fault
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An earthquake is not: … a giant crack that opens up and swallows buildings whole …like an underground explosion … defined by a point in space or time … easily predictable
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Fault: A surface across which two blocks can move relative to each other.
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San Andreas Fault Trace, California
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Focus: The location on a fault where earthquake rupture initiates.
Focal depth
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Hypocentre: The calculated position of an earthquake focus.
(almost synonymous)
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Epicentre: That point on the Earth's surface directly above the hypocentre.
Epicentral Distance
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Seismic Waves 101 Body waves Fast Slow P waves
Primary (or compressional) S waves Secondary (or shear) Surface waves Love waves Rayleigh waves
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Northern Peru, Magnitude 7.5
SS P Rayleigh S ELFO 6.6 min 2005/09/26 01:55: km depth
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Estimating Epicentral Distance (D)
For a distant earthquake: D ~ 1000 Dt Dt in minutes, D in km For a local earthquake: D ~ 8 Dt Dt in seconds, D in km Dt e.g., D ~ 1000* = 5100 km Note: Just a crude estimate!
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Earthquake epicentres are located by triangulation
Requires Dt from at least 3 stations
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Magnitude: A measure of the strength of an earthquake, as determined by seismographic observations.
Different magnitude formulas are used. Examples: Richter magnitude Surface-wave magnitude
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Small earthquakes happen often, but large earthquakes are infrequent...
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Surface-wave magnitude formula
(most common) MS = log10(A) log10(D) A = amplitude in microns (mm) D = epicentral distance in degrees (divide by 111 to go from km to degrees)
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Magnitude Calculation
672 mm Magnitude Calculation Example D ~ (5100/111) ~ 46 degrees MS = log10(A) log10(D) = 7.4
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