Strike-slip (transcurrent) faults.
Oblique faults exhibit some strike-slip movement, but they also have a dip-slip component.
A transform fault boundary if I'm not mistaken. The San Andreas fault is actually a "transform" fault, which means that the movement of the plates is a side-to-side movement past each other. The Pacific plate, relatively speaking, is moving north and the North American plate is moving south. This means that the very western coast of California is sliding north past the rest of California.
A normal fault is the result of the downward movement of rock along the fault line.
they cause the world to spin
The San Andreas fault is a right-lateral (dextral) strike-slip fault which marks a transform (or sliding) boundary between the Pacific Plate and the North American Plate. In essence the plate boundary is destructive rather than constructive but at present the energy is directed at moving the Pacific Plate in a generally northerly direction, parallel with the coastline.
If a fault occurs in an area where rock layers have been folded, the type of fault it is likely to be is thrust faulting. This type of fault will have the ground on one side of the fault, move up and over adjacent ground.
hgvuygyug
A backwards one. -_-
A transform fault boundary if I'm not mistaken. The San Andreas fault is actually a "transform" fault, which means that the movement of the plates is a side-to-side movement past each other. The Pacific plate, relatively speaking, is moving north and the North American plate is moving south. This means that the very western coast of California is sliding north past the rest of California.
A normal fault is the result of the downward movement of rock along the fault line.
A fault is, generally speaking, a fracture in a rock formation which indicates crustal movement on either side. A fault is a specific type of rock fracture, for which there are many causes.
thrust A+
thrust A+
they cause the world to spin
The type of rock layers found on one side of the fault will either be repeated higher or lower on the other side of the fault. This proves that one side of a fault has moved (slipped).
The San Andreas fault is a right-lateral (dextral) strike-slip fault which marks a transform (or sliding) boundary between the Pacific Plate and the North American Plate. In essence the plate boundary is destructive rather than constructive but at present the energy is directed at moving the Pacific Plate in a generally northerly direction, parallel with the coastline.
that would be the shoulder
Dip-slip faults is the term used for any fault that has movement in the vertical direction. One side moves up where as the other side moves down. Examples are Normal Fault and Reverse fault.