Two graphics showing reverse/thrust faulting, and strike-slip faulting.
The three principal fault types are strike-slip,
reverse, and normal (see fig. 5). Movement occurs along a fault plane. Footwalls are below the fault plane, and hanging walls are above. In a normal fault (see fig. 5), crustal extension (pulling apart) moves the hanging wall down relative to the footwall. Faults mapped in the vicinity of the monument are normal faults. In a reverse fault, crustal compression (squeezing together) moves the
hanging wall up relative to the footwall. A thrust fault is a type of reverse fault that has a dip angle of less than 45°. In a strike-slip fault, movement is horizontal. When movement across a strike-slip fault is to the right, it is a right-lateral strike-slip fault, as illustrated above. When movement is to the left, it is a left-lateral strike-slip fault.
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Graphic by Trista Thornberry-Ehrlich (Colorado State University).
Public domain:Full Granting Rights
Image
Casa Grande Ruins National Monument, Code: CAGR
Casa Grande Ruins National Monument, Pinal County, Arizona Latitude: 32.996898651123, Longitude: -111.532997131348