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How does rock respond to stress?

A fault is a absent fracture where the two sides have been displaced relative to each other.Faults space categorized right into three general groups based on the feeling of slip or movement.

SEE TABS over for stand-alone version of every fault type.

This clip has selected excerpts native the more-in-depth animation, "Earthquake Faults, bowl Boundaries, & Stress"

Normal faultthe block above the skinny fault moves down family member to the block below the fault. This fault movement is resulted in by extensional forces and results in extension. instances include container & selection faults.

Reverse faultthe block over the skinny fault moves up family member to the block below the fault. This fault motion is caused by compressional forces and also results in shortening. A turning back fault is dubbed a thrust fault if the emboldened of the fault aircraft is small. Examples include the Rocky Mountains and also the Himalayan Mountains.

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Strike-slip fault—movement the blocks follow me a error is horizontal and the fault airplane is almost vertical. If the block on the far side of the fault moves to the left, as displayed in this animation, the error is called left-lateral (Figure 2). If it move to the right, the fault is dubbed right-lateral. The fault activity of a strike-slip fault is led to by shearing forces. Examples incorporate the san Andreas Fault, California; Anatolian Fault, Turkey.