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GEO ch 7
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Deformation
Tensional forces
Compressive forces
Shearing forces
tension forces occurs at
divergent boundaries
strike and dip
describe the orientation of rock layer exposed at an outcrop
compass direction of rock layer
strike
dip
amount of tilting
geologic cross sections
diagrams showing the features that would be visible if verticle slices were made through part of the crust
brittle deformation produces
faults
dipslip fault
fault on which there has been relative movment of blocks of rock up or down the dip of the fault plane
extension produces
normal fault
basin
bowlshaped depression of rock layers
dome
broad circular upward bulge of rock
Author
xryan27x
ID
140451
Card Set
GEO ch 7
Description
geo
Updated
2012-03-08T05:35:33Z
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