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Earthquakes

7th Grade Science, Inside Earth

AB
seismic wavescarry energy from and earthquake away from the focus
earthquakethe shaking that results when rocks move inside Earth
focusthe place where rocks break and cause an earthquake
epicenterthe point on the surface directly above the focus
3 kinds of seismic wavesP waves, S waves, surface waves
P wavesmove rocks back and forth; fastest seismic waves; arrive first
S wavesmove rocks up and down; travel more slowly than P waves; arrive second
surface waveswaves that travel along Earth's surface; the slowest seismic waves that cause the most damage
3 methods of measuring earthquakesMercalli scale, Richter scale, moment magnitude scale
Mercalli scalemeasurement based on the amount of damage an earthquake does
Richter scalemeasurement based on the size of the seismic waves
seismographan instrument that measures the size of seismic waves
moment magnitude scalemeasurement based on the amount of energy an earthquake releases
epicenterthe point on Earth's surface that lies directly above an earthquake's focus
finding the location of the epicenterto do this, you need seismographs in three different places
seismograph readingsthese can tell you whether an earthquake is closer or farther away
instruments that monitor faultsthese measure changes in Earth's elevation, tilting of the land surface, and ground movements along faults
clues that an earthquake might happenground movements near a fault
instruments tht monitor faultstiltmeters, creep meters, GPS satellites
tiltmetershows how much the Earth is tilting or tipping
tiltmeterthis instrument measures when the ground tilts; water inside a glass bulb shows how much tilting there is
creep meterthis instrument shows how far the sides of a fault have moved in the opposite directions
creep meterthis instrument uses a wire stretched across the fault; the wire gets longer when the two sides move apart
GPS satellitesmarkers are put on both sides of a fault do detect tiny movements in any direction along a fault
a place where an earthquake is likelywhen stress builds up at faults where rocks do not move easily
what happens to seismic waves when they reach a faultseismic waves bounce off a fault like a ball bouncing off a wall


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