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Geology

Terms

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Elastic rebound theory
"faults remain locked while strain energy accumulates in the rock formation on both sides, temporarily deforming them until a sudden slip along the fault releases the energy"
Epicenter
the point at the surface directly above the focus
Fault
locus of the earthquake movement, come in all scales
Focus
site of initial rupture (usually at depth)
Liquifaction
sudden loss of strength of water-saturated sediment; buildings fall down intact
Love Wave
shear vibrations in the horizontal plane (side-to-side, shaking motion)
P Waves
(compressional-primary) Parallel to direction of movement, also called primary waves. Similar to sound waves
Rayleigh Wave  
shear and compressional vibrations in both the horizontal and vertical planes
S Waves  
(shear, secondary) perpendicular to direction of movement, also called secondary waves, result from shear strength of material--do not move through liquid  
Seismic Waves
a general term for the elastic waves produced by earthquakes and explosions
Seismology
study of the propagation of mechanical energy; released by earthquakes and explosions through the Earth
Slip
the distance of displacement along the fault

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