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Earthquakes & Earth’s Interior

AB
AftershockSmaller earthquakes that follow a large one.
AsthenosphereWeak layer in the upper mantel with a small amount of melting.
Body WaveWaves that travel with in the earth.
CrustThin outer layer of the earth
EarthquakeA vibration in the earth because of a rapid release of energy.
Elastic ReboundThe springing back of the Earth to its primary position.
EpicenterLocation on the surface directly above the focus.
FaultFractures in the Earth’s surface.
Fault CreepSlow gradual displacement of the fault.
FocusThe location of the earthquake.
ForeshockSmall earthquakes that will precede a large one.
Inner CoreSolid metal center of the planet.
LiquefactionWhere stable soil becomes an unstable liquid.
LithosphereSphere of rock located on the outside.
MagnitudeThe power of something.
MantleThick rocky layer underneath the crust.
Mercalli Intensity ScaleOld scale the determined earthquakes strength based on destruction that it caused to buildings.
Moho DiscontinuityBoundary that separates the crust for the underlying layers.
Outer CoreMobile core that is made of a liquid.
Primary (P) WavePush Pull waves that can travel though all materials.
Richter ScaleScale that is used by determining the amplitude of the earthquake.
Secondary (S) WaveShake wave cannot travel in gases or liquids.
Seismic Sea Wave (tsunami)A large wave of water caused by an earthquake.
SeismogramRecords of earthquakes that exhibit the waves.
SeismographInstruments that read and record earthquakes.
SeismologyStudy of earthquakes.
Shadow ZoneA zone 35 degrees where the P wave disappears.
Surface WaveWaves that travel along the surface.


Middle School Science Teacher
Clinton/Graceville/Beardsley Middle School
Beardsley, MN

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