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Seismology is the study of
Earthquakes
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Earthquake in Turkey in 2001 buckled railroad ties
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Armenia Earthquake 1988
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Great Alaska Earthquake 1964 8.9
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East Coast Earthquake 5.8
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Mercalli Damage Scale
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Richter Scale - each increase of 1 represents 10 times
more energy
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9.0 Sumatra 2004 8,9 Japan 2011 8.8 Chile 2010 7.0 Haiti 2010 5.8 Virginia 2011
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focus animation
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Earthquakes produce 3 types of waves
Ground roll P wave
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wave motion 1 p wave motion s wave motion
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Differences between “P” and “S” waves
P Waves travel almost twice as fast P waves travel through liquids and solids P waves all called primary waves or push -pull -waves S waves cannot travel through liquids S waves provide evidence for a liquid outer core S waves are called shear waves or secondary waves
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L waves (or ground roll) can be the
Biggest. They travel along the surface and Cause a lot of the surface damage
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P and S waves travel throughout the earth
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When the waves enter a zone of sharply differing density, they are bent or refracted. This causes SHADOW ZONES
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refraction shadow zones shadow zones 2
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The waves are received on a seismograph
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Seismometer
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Simplified version of seismographs
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Most earthquakes occur along ACTIVE FAULTS at tectonic plate boundaries
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Pacific Plate San Andreas Fault N. American Plate
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Socal Earthquakes
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A branch of the San Andreas
Fault running across highway
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Earthquake along San Andreas Fault
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