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Faulting and Folding

These activities will build and reinforce basic vocabulary skills that will help in understanding how different types of stress cause the faulting and folding that build mountains, valleys and plateaus.

AB
stressforces that push and pull on the Earth's crust, causing deformation
crustthe surface layer of the earth
deformationa change in the original shape or volume of rock
compressionstress that squeezes rocks together
tensionstress that pulls rocks apart
shearingstress that pushes rocks in two opposite horizontal directions
fracturea break or crack in rocks
faulta break or crack along which rock move
hanging wallthe block of rock above a fault
footwallthe block of rock below a fault
normal faultfault in which the hanging wall moves down
reverse faulta fault in which the hanging wall moves up
thrust faulta reverse fault in which the hanging wall slides over the foot wall
lateral faulta fault along which the blocks move horizontally past each other
corethe center of the earth
folda bend in rock
anticlinean upward fold in rock
synclinea downward fold in rock
plateaua large area of flat land that is raised high above sea level
dome mountaina raised area formed by magma pushing upward on rock layers
mantlethe layer of the earth that extends from the core to the crust
fault-block mountainmountain formed by blocks of rock uplifted from normal faults
isostasythe balancing of the downward force of the crust and the upward force of the mantle
rift valleylow area formed when the land between two normal faults slides downward


Family and Consumer Science, Instructor
Cleveland High/Cleveland Middle School
Cleveland, TN

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