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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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