surface along which rocks move when they pass their elastic limit
Earthquake
vibrations produced when rocks break along a fault
Normal Fault
break in rock caused by tension forces, where rock above the fault surface moves down relative to the rock below the fault surface
Reverse Fault
break in rock caused by compressive forces, where rock above the fault surface moves upward relative to the rock below the fault surface
Strike-Slip Fault
break in rock caused by shear forces, where rocks moves past each other without much vertical movement
Focus
The point below the Earth’s surface where energy is released in the form of seismic waves
Seismic Wave
wave generated by an earthquake
Primary Wave (P-Wave)
seismic wave that moves rock particles back and forth in the same direction that the wave travels. These waves travel fastest and arrive first.
P- Wave
Secondary Wave (S-Wave)
seismic wave that moves rock particles at right angles to the direction of the wave. These waves arrive second.
S- Wave
Comparison P-Wave S-Wave
Surface Wave
Seismic wave that moves rock particles up and down in a backward rolling motion and side to side in a swaying motion. These waves arrive last and are the most destructive.
Damage Video
Epicenter
point on Earth’s surface directly above an earthquake’s focus
Seismograph
Instrument used to register earthquake waves and record the time that each arrived
Magnitude
The power of an earthquake. Measured by the Richter Scale (1-10)
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