Faults

Dip-Slip Fault

Normal Dip-Slip Fault

"In a normal fault, the block above the fault moves down relative to the block below the fault. This fault motion is caused by tensional forces and results in extension. [Other names: normal-slip fault, tensional fault or gravity fault]"

Strike-Slip Fault

 

 

"In a strike-slip fault, the movement of blocks along a fault is horizontal. If the block on the far side of the fault moves to the left, as shown in this animation, the fault is called left-lateral. If the block on the far side moves to the right, the fault is called right-lateral. The fault motion of a strike-slip fault is caused by shearing forces. [Other names: transcurrent fault, lateral fault, tear fault or wrench fault]"

Reverse Dip-Slip Fault "In a reverse fault, the block above the fault moves up relative to the block below the fault. This fault motion is caused by compressional forces and results in shortening. A reverse fault is called a thrust fault if the dip of the fault plane is small. [Other names: thrust fault, reverse-slip fault or compressional fault]"

Oblique Fault

"Oblique-slip faulting suggests both dip-slip faulting and strike-slip faulting. It is caused by a combination of shearing and tension of compressional forces."

 

http://www.iris.edu/gifs/animations/faults.htm

Earthquake Search

Loading

Use this custom search box to help find more useful information on Earthquakes.