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EARTHQUAKES Information from the USGS
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Locations of Earthquakes Dots are earthquakes
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Locations of Earthquakes Earthquakes occur in a pattern
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Tectonic Plates Pattern of earthquakes follows plate boundaries You are HERE
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Tectonic Plates There are ~23 major plates
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Plate Boundaries Three types of interactions between plates as they move around
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Plate Boundaries Sliding past one another - transform boundary
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Plate Boundaries Running into one another - convergent boundary
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Plate Boundaries Moving away from one another - divergent boundary
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3 Types of Faults Form depending on: –type of plate motion –complex reaction of earth’s lithospheric blocks
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3 Types of Faults Strike-slip fault
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3 Types of Faults Normal fault
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3 Types of Faults Thrust
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Examples of Faults Strike-slip fault
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Examples of Faults Strike-slip fault: 1906 San Francisco Manure pile Old position of pile
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Examples of Faults Strike-slip fault: 1906 San Francisco
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Examples of Faults Normal fault: DOWN Fairview Peaks, NV 1954
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Examples of Faults Thrust fault: UP
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Slip Happens Slip is the amount of movement in any given place.
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Slip Happens Slip is the amount of movement in any give place. Slip is NOT equal throughout an earthquake zone
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See Slip Here is a cross-section of “slip” during a ‘quake. Blue = none, Red = a lot
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Slip Happens Slip changes over the time span of the earthquake event
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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 fault START
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Slip on an earthquake fault Second 2.0
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Slip on an earthquake fault Second 4.0
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Slip on an earthquake fault Second 6.0
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Slip on an earthquake fault Second 8.0
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Slip on an earthquake fault Second 10.0
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Slip on an earthquake fault Second 12.0
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Slip on an earthquake fault Second 14.0
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Slip on an earthquake fault Second 16.0
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Slip on an earthquake fault Second 18.0
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Slip on an earthquake fault Second 20.0
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Slip on an earthquake fault Second 22.0
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Slip on an earthquake fault Second 24.0
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