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Seismic waves are elastic waves. Four types: 2 Body Waves.

Seismic waves are elastic waves. Four types: 2 Body Waves. So called because they travel through the Earth. These are P & S waves. P = primary S = secondary or shear 2 surface waves . So called because they travel primarily on surface. These are Love waves and Rayleigh waves.

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Seismic waves are elastic waves. Four types: 2 Body Waves.

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  1. Seismic waves are elastic waves. Four types: 2 Body Waves. So called because they travel through the Earth. These are P & S waves. P = primary S = secondary or shear 2 surface waves. So called because they travel primarily on surface. These are Love waves and Rayleigh waves.

  2. Two types of Surface Waves

  3. Wavefronts and rays

  4. Period, amplitude and frequency Equations for Vp and Vs

  5. Vp ~ 1.7 Vs

  6. Since Vp > Vs > Vsw P waves generally arrive at a station first.

  7. Mag 6.9 Earthquake in Kamchatka Recorded in Mount Soledad

  8. What happen when the ray/wave hits an interface?

  9. Snell’s Law:

  10. What happens to waves in the Earth? Density increases due to pressure but so do the bulk and shear moduli. Therefore rays bend!

  11. P-wave SZ is between 104° and 140°. S-wave SZ between 104 ° and 256°

  12. Labeling Waves. P = direct P S = direct S p = P-wave that travels up first s = S-wave that travels up first PP = One bounce at surface of P wave SS = One bounce at surface of S wave c = reflection from core K = P wave through outer core I = P wave through inner core i = P wave refected from inner core J = S wave through inner core Combine: PcP = P wave that bounces off outer core and goes to surface PcS = P wave that bounces off outer core and converts to S which Travels to the surface ScS = S wave that bounces off outer core and goes to surface etc

  13. Show movies. Homog.1.aviPrem-path.aviRaypath.avi

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