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Published byΠαλλάς Δημαράς Modified over 6 years ago
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Earthquakes
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San Andreas Fault The 800-mile (1,300-kilometer) fault runs through western and southern California, dividing the Pacific and North American plates
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Compression Waves aka P-Waves
Fastest Waves – arrive first (primary waves) Push – Pull rocks in the same direction as the wave travels Travel through solids and liquids (Travels through entire earth Theoretical p-waves travel times
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Shear waves aka S-waves or Secondary Waves
Body waves characterized by a series of sidewise or shearing movements causes particles to move at right angles to wave direction Slower than P-waves Can travel through solid material only
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Animation of p-waves and s-waves
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Surface Waves Love waves (L-Waves) Rayleigh Waves
Move in two directions as they pass through the surface Up and Down as well as Side to Side CAUSE THE MOST DAMAGE TO BUILDINGS
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3-D Models
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Seismograph or Seismometer
instrument that records the intensity and duration of earthquakes and similar tremors
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Seismogram The record produced by a seismometer
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