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Volcanoes and Earthquakes

Review for chapter 8 & 9

AB
seismologythe study of earthquakes
faulta break in the Earth's crust along which block of the crust slide relative to one another
deformationthe change in the shape of rock in response to stress
elastic reboundthe sudden return of elastically deformed rock to its original shape
reverse faultscauses strong deep earthquakes
normal faultscauses weak. shallow earthquakes
strike-slip faultcauses moderate, shallow earthquakes
seismic waveswaves of energy that travel through the Earth
body wavesseismic waves that travel through the Earth's interior
P wavestravel through solids, liquids, and gases
S wavesshear back and forth, secondary waves
surface waveswaves that move the ground up and down
siesmographsinstrument that detects earthquakes
seismograma tracing of earthquake motion
epicenterthe point on the Earth's center directly above the earthquake's starting point
focusthe point inside the Earth where the earthquake begins
volcanoa mountain that forms when molten rock is forced to the Earth's surface
lavamagma that flows onto the Earth's surface
explosive eruptionclouds of hot debris and gases shoot out from the volcano
What causes a volcano to be explosivehigh water content, silica rich magma
ventsholes in the Earth's crust
magma chamberarea in the earth where the magma is stored
pyroclastic materialrock fragments created by explosive volcanic eruptions
shield volcanononexplosive eruptions
cindercone volcanomade of pyroclastic material, erodes quickly
composite volcanothe most common type of volcanoes
craterfunnel-shaped pit at the top of the volcano
calderasforms when a magma chamber empties and its roof collapses
rifta deep crack
hot spotsplaces on the Earth's surface direct above mantle plumes
tiltmetermeasures the slope of volcanoes


Earth Science
Risley Middle School
Brunswick, GA

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