Earthquakes
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Transcript of Earthquakes
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Earthquakes
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Most earthquakes occur at Plate Boundaries
The deepest earthquakes occur at subduction boundaries
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The focus of an earthquake is the source, or where it originates.
The epicenter is the point on the Earth’s surface directly above the focus.
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Types of Seismic Waves P- Waves (elastic) – push and pull the
ground• Travel through solids,liquids & gases
S-Waves (shear) – move the ground up and down. • Only travel throughsolids
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Types of Seismic Waves L-waves (rolling surface waves)-
arrive last; move ground up and down and to the side• Only travel through solids
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Seismographs record results on seismograms
The difference in arrival times of p and s waves= lag time• Using lag time we can find the distance to
the epicenter
Recording Earthquakes
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Recording Earthquakes The further away the seismograph
station, the greater the lag time.
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Recording Earthquakes We need 3 seismograph stations to
find the epicenter of an earthquake. • With one, it could be anywhere on the
circle.• With two, it could be either two areas they
touch.• With three, its where they all meet!
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Why plate boundaries?? This is where the crust is under stress
and potential energy is stored.
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Magnitude Measure of how much energy is
released.
Richter scale is used to plot, from 1 – 10, how strong an earthquake is.
Each increase in 1 equals 10 times more energy released.
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Travel-Time Graphs Used to record the distance
(measured in km) from the recording center to the epicenter of an earthquake