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Stresses, Faulting, and Folding

Your knowledge of the study guide and more will help you answer each question.

AB
stressa force that acts on rock to change its shpe or volume
types of stresstension, compression, and shearing
action of tensionstretches rock so that it becomes thinner in the middle
action of shearingpushes masses of rock in opposite directions, in a sideways movement
action of compressionrock is squeezed until it folds or breaks
faulta break in Earth's crust where masses of rock slip past each other
location of most faultsplate boundaries
types of faultsnormal, reverse, thrust, strike-slip
normal faulthanging wall moves down
reverse faulthanging wall moves up
thrust faulthanging wall moves up and over foot wall
strike-sliphanging wall and foot wall slip sideways past each other with little up or down motion
folda bend in the rock
anticlinean upward fold
synclinea downward fold
plateaua large area of flat land elevated high above sea level


Earth Science & Life Science Teacher
Concord Middle School
Concord, MA

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