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Science Study Guide

Terms

undefined, object
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elastic limit
how far rocks can be stretched, or bent. when passed earthquakes occur
surface waves
(L-waves) slowest waves, make rocks move in a rolling motion, and a side to side swaying motion **causes the most damage**
primary waves
(P-waves) fastest waves, cause rocks to compress and then spread apart (stretching and letting go of a slinky) slow down when they go through liquid
fault
rocks move along these surfaces after they get stretched passed their elastic limit
focus
the point of energy release in an earthquake
epicenter
the poit on the earths surface directly above the focus
secondary waves
(S-waves) second waves,cause rocks to move at right angles to the direction of the wave travel **moves like waves on a beach** can't travel through liquid
normal fault
foot wall up, hanging wall down
seismograph
instrument used to record seismic waves from an earthquake they consist of a rotating drum of paper and a pendulum with an attached pen, when seismic waves reacj the seismograph the drum vibrates but the pendulum remains at rest, the pen traces a record of the vibrations on the peice of paper
seismologist
scientist that studies earthquakes
strike slip fault
rocks on either side of the fauld move past each other without much upward or downward motion
seismic waves
waves of motion created by an earthquake that travel through earth
earthquake
the vibrations produced by the breaking of rock
reverse fault
foot wall down, hanging wall up

Deck Info

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