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where do eqs happen
95% along plate boundaries
shallow depth
<70km (divergent and transform)
deep focus
>70 km (convergent)
stress
force acting on crustal rocks that causes rock to be deformed - movement of Earth occurs when stress on rocks is greater than the strength of rocks
compression stress
decreases material volume (squeezes)
tension stress
pulls material apart
shear stress
different parts of material moved in different directions
strain
deformation of material in response to stress
elastic deformation
when material is compressed, bent, or stretched; occurs under low stress; rock returns to original state when stress is gone
plastic deformation
strain that produces permanent damage,
fault
crack in Earth’s crust along which rock has moved
elastic rebound
release of strain energy as rocks move along fault
What happens when rocks are deformed by stress?
strain energy builds up and energy can be released if stress large enough to overcome the strength of the rocks
seismic waves
vibrations of the ground produced during an eq
epicenter
point on Earth’s surface above the focus
-surface waves originate here
focus
point where body waves originate
primary wave (p wave)
squeeze and push rocks in the same direction that the waves are traveling; fastest waves, travel through solids and liquids
secondary wave (s wave)
moves at right angles (up and down) to the direction of the wave; named for arrival time; slower than p waves, only travel through solids
surface waves
only on earth’s surface, slowest type of wave; usually the most destructive- cause the most movement of the ground and take the longest time to pass
rayleigh wave
move up and down
long wave
move side to side
mercalli scale
qualitative observation; measured based on the intensity of eq
ritcher scale
quantitative, numerical measurement of magnitude of eq (amplitude - energy)
seismometer
instrument used to measure motion of the ground during an earthquake
seismograph
record produced by a seismometer