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| Extension, stretching stress |
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| Each side is sliding past each other |
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| Can result in joints and faults |
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| rock sheared at great depth or high temperature (heat) |
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| each side slides past each other with motion parallel to the fault |
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| each side of the fault moves up or down the dipping fault surface |
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| as a response to compressive stresses |
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| imaginary plane that cuts through the hinges of successive rock layers |
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| fractures along which there is NO movement |
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| fractions along where there is movement |
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| kind of reverse fault where fault plane dips less than 30 degrees |
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| uplifted rock bounded by normal faults |
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| down- dropped block bounded by normal faults |
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| exposure of the fault surface |
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| amount of offset or slip on a fault |
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| powdered rock in a fault zone |
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| shattered rock caused by fault movements |
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