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F5: Earthquakes

Vocabulary practice for Holt, Rinehart and Winston science

AB
seismologythe study of earthquakes
seismologista person who studies eartquakes
faulta break in the Earth's crust in which plates slide past one another
deformationa change in the shape of rocks due to stress
plastic deformationrocks act like a piece of molded clay; does NOT cause earthquakes
elastic deformationrock stretches and snaps back like a rubber band; this causes earthquakes
elastic reboundsudden return of elasticall deformed rock back to its original shape
Transform plate motioncauses a strike slip fault
Convergent plate motioncauses a reverse fault
Divergent plate motioncauses a normal fault
earthquake zonea place where a large number of faults are located
seismic waveswaves of energy that travel through the Earth
body wavesP waves and Swaves are a type of these
survace waveswaves of energy that travel along the Earth's surface
pressure wavesP waves or primary waves
shear wavesS waves or secondary waves
P wavesseismic wave that causes rock to move in a back- and- forth direction
S wavesseismic wave that causes rock to move in a side-to-side direction
seismographan instrument that records vibrations in the ground and determines strength and location of an earthquake
seismograma tracing of earthquake motion that is created by a seismograph
epicenterpoint on the earth's surface diectly above an earthquakes starting point
focusthe point along a fault at which the first motion of an earthquake occurs; it is inside the Earth
S-P time methoda method for finding the epicenter of an earthquake
Richter Magnitude Scaleused to measure strength of a quake
magnitudea measure of the strength of a quake
intensitymeasure of the degree to wich an earthquake is felt and the damage that it causes
Mercalli Intensity Scaleused to measure damage caused by an earthquake
earthquake hazardmeasure of how likely an area is to have a damaging earthquake in the future
gap hypothesissays that a major earthquake is more likely to occur along a path of an active fault where no earthquakes have occured for a period of time
seismic gapan area where few earthquakes have occured recently, but
retrofittingthe process of making older structures more earthquake resistant
mass damperweight on the roof of a building
active tendon systemfound at a lower level in a building. works like a mass damper.
base isolatorsact like shock absorbers, they absorb seismic waves so they do not travel through the building
cross bracesplaced between the floors of a building;counteract pressure that pulls and pushes through a building
flexible pipesprevent waterlines and gas lines from breaking


St. James Catholic School
Millstadt, IL

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