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Earthquake Activities

Th following activities will help you prepare for your "Earthquakes" test. Content is intended for grade 8 only.

AB
StressForces that change shape and volume of rock
TensionForce that stretches crust
CompressionForce that squeezes crust
ShearingForce that makes plates slide past each other
NormalFault resulting from tension force where plates split and rock slips over other rock
ReverseFault resulting from compression force where rocks push and plate slides over other
Strike SlipFault that results from shearing, slips past each other
AnticlineCaused by compression, folds rock upward
SynclineCaused by compression, bends rock downward
PlateauHighly elevated land with a flat top
Folded MountainsFormed from compression, high elevation, high relief
Fault Block MountainsFormed from tension. Mountains are separated with valleys and basins
EarthquakeShaking and trembling on earth’s surface due to plate movement and rocks breaking
FocusWhere rock breaks in lithosphere
EpicenterArea above focus on earth surface
P Wave1st to arrive, compress back and forth, initial jolt
S Wave2nd to arrive, shake from side to side and up and down (wave like motion), shake ground
Surface waveFormed on surface, slowest, ground rolls, severe ground movement
Mercalli ScaleRates earthquakes based on level of damage on surface 1-12
Richter ScaleRates earthquake based on seismic data from seismograph
Moment Magnitude ScaleMeasures total energy released, good for near and far, small and large quakes
SeismographInstrumenused to collect seismic data
LiquefactionShaking of ground from earthquake causes moisture-rick soil to liquefy like quicksand
AftershockFrom same focus area, additional shaking because plate still adjusting, can happen minutes, hours, days later, can be more damaging because land is already unstableFrom same focus area, additional shaking because plate still adjusting, can happen minutes, hours, days later, can be more damaging because land is already unstable
TsunamiLarge tidal wave due to water displacement from underwater earthquakes



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