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Chapter 2 Movement of the Earth's Crust

stress, faults, and earthquakes

AB
stressthe push pull force on the Earth's crust, changes the volume and shape
three types of stresscompression, tension, shearing
compressionwhenrocks are squeezed together, pushes rocks up or down
tensionwhen rocks are pulled apart, thinner in the middle
shearingrocks are pushed in opposite, horizontal directions
faulta break or crack along which rocks move
jointscracks from rock fractures
hanging wallblock of rock above a fault
foot wallblock of rock below a fault
normal faultcaused by tension, hanging wall moves down
reverse faultfrom compression, hanging wall moves up
thrust faultfrom compression, hanging wall slides over foot wall, older rocks pushed on top
lateral faultone block moves left or right of second block
deformationthe fold, fault, or tilt due to stress
fault block mountainsnormal faults form a series of mountains
rift valleysa block of land between 2 normal faults slides downward
foldinga bend in a rock, ex, Appalachian Mtns
anticlinean upward fold
synclinea downward fold
causes of foldingtemp.hot, rocks will fold, pressure great=fold
ductile rocksbendable rocks that will fold
brittle rocksmore likely to fault
gradual forcerocks will fold
sudden forcerocks will fault
Mercalli scalenot precise, rates by intensity, tells how affects people, buildings, land
Richter scalemeasures strength from 1 to 10, local earthquakes only
Moment magnitude scalemeasures total energy released, scale of 1 to 10
epicenterpoint on the crust above the focus
focusunderground point of origin
p wavesprimary waves travel the fastest, compressional wave
s wavessecond wave to reach surface, up and down waves
surface wavesroll along on surface, bend/twist surface of earth, slowest wave
seismic waveearthquake waves, travel outward
seismographinstrument that measures seismic waves
liqueficationsoft soil turns into mud, triggers landslides
aftershocksearthquakes that occur after a large earthquake
tsunamitidal waves from earthquakes which occur beneath ocean floor
base isolated buildingsreduces energy from earthquake, building is build on shocks
creep meterswire stretched across fault, measures horizontal movement
laser devicelaser beam which detects fault movements
tiltmetermeasures tilting of ground, lever with two bulbs fulled with liquid
satellite monitormakes pictures of the fault, distance from ground to satellite is recorded
plateauflat topped rocks,high above sea level
domesmagma pushes up over rock layers, Black Hills


Mrs. McSheffrey

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