The San Andreas Fault in California is a transform fault. In a transform fault, two lithospheric plates are grinding alongside each other in different directions. Friction between the plates causes points along the fault to get 'hung up'. When the friction between the plates exceeds the maximum elasticity of the rock, the tension is released, the plates snap into their new positions, and an earthquake occurs.
Srike slip fault
transform fault
It is on a transform fault boundary.
It is a right-lateral strike-slip fault
The San Andreas Fault is an example of a transform boundary in which plates slide past each other. This type of fault may also be known as a strike slip fault. During this plate motion, lithosphere is neither created nor destroyed. Shear stress causes the undeformed block of rock to experience tearing and smearing.The San Andreas fault is actually a "Strike-Slip" 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. The San Andreas fault is a strike-slip fault
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.
transform fault
Strike-Slip fault is the most common fault type in the San Andreas fault system.
On a fault line. For example, California is on the San Andreas fault, and as such is very earthquake prone.
It is a THRUST fault The San Andreas Fault
I believe it is called a fault, like the San Andreas fault in California.
Strike-slip faults are the most common fault type around the San Andreas Fault.
It is on a transform fault boundary.
A transverse fault
Transform Boundary
It is a right-lateral strike-slip fault
Platetectonics, from the pacific going down under the u.s.
The San Andreas Fault is an example of a transform boundary in which plates slide past each other. This type of fault may also be known as a strike slip fault. During this plate motion, lithosphere is neither created nor destroyed. Shear stress causes the undeformed block of rock to experience tearing and smearing.The San Andreas fault is actually a "Strike-Slip" 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. The San Andreas fault is a strike-slip fault