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Chapter 8 Vocabulary

AB
faultsurface along which rocks break and move
earthquakevibrations caused by breaking rocks along faults; most result from plates moving over, under, and past each other
normal faultbreak in rock due to tension forces, where rock above the fault surface moves downward in relation to rock below the fault surface
reverse faultbreak in rock due to compression forces, where rocks above the fault surface move upward and over the rocks below the fault surface
strike-slip faultbreak in rock due to shearing forces, where rocks on either side of the fault surface move past each other with little upward or downward movement
seismic waveenergy waves that are produced at and travel outward from the earthquake focus
focusin an earthquake, the point beneath Earth's surface where energy release occurs.
primary wavewaves that travel outward from an earthquake's focus and cause particles in rocks to move back and forth in the same direction the wave is moving
secondary wavewaves that travel outward from an earthquake's focus and move through Earth by causing particles in rocks to vibrate at right angles to the direction of the wave
epicenterpoint on Earth's surface directly above an earthquake's focus
surface wavewaves of energy that reach Earth's surface during an earthquake, travel outward from the epicenter, and move rock particles up and down and side to side
inner corevery dense, solid center of Earth that is made mostly of iron with smaller amounts of oxygen, silicon, sulfur, or nickel
outer coreliquid core that surrounds Earth's solid inner core and that is made mostly of iron
mantlelargest layer inside Earth, lying directly above the outer core and that is made mostly of silicon, oxygen, magnesium and iron.
crustEarth's outermost layer, which varies in thickness from about 5 km to 60 km and is separated from the mantle by the Moho discontinuity
seismologistscientist who studies earthquakes and seismic waves
seismographdevice used by seismologists to record primary, secondary, and surface waves from earthquakes
magnitudemeasure of the energy released by an earthquake
tsunamipowerful seismic sea wave that can travel thousands of kilometers in all directions and that begins over an earthquake focus

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