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