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Earthquakes & Earth’s Interior

Glencoe Earth Science Chapter 11 Earthquakes

AB
AftershockSmaller earthquakes that follow a large one.
AsthenosphereWeak layer in the upper mantel with a small amount of melting.
Reverse Faultbreak in rock caused by compressive forces, where rock above the fault surface moves upward relative to the to the rock below the fault surface
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.
Normal Faultbreak in rock caused by tension forces, where rock above the fault surface moves down relative to the rock below the rock surface
FocusThe location of the earthquake.
Strike-slip Faultbreak in rock caused by shear forces, where rocks move past each other without much vertical movement
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.
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.
Surface WaveWaves that travel along the surface.

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