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San-Andreas fault.
Some examples of strike-slip faults include the San Andreas Fault in California, the Anatolian Fault in Turkey, and the Great Glen Fault in Scotland.
Slip-strike faults always occur at transform boundaries. The San Andreas Fault is a famous transform boundary in located in southern California.
Dip-Slip fault is a bedding fault and its pattern is En-Echelon, while Strike Slip fault is strike fault and its pattern is Parallel.
San Andreas fault
The Hayward Fault is a Strike-slip Fault.
A strike-slip fault occurs at a transform boundary. It is created when stress is added to rock, in this case the stress that is on the rock is called shearing. A fault is simply a crack in the Earth's crust, and strike-slip fault is when the two pieces of crust are sliding past one another horizontally. An example of a strike-slip fault is the San Andreas Fault in California.
Dip-Slip fault is a bedding fault and its pattern is En-Echelon, while Strike Slip fault is strike fault and its pattern is Parallel.
Strike slip fault - Look it up!
strike-slip
strike-slip has a horizontal motion
No. It is a strike-slip fault.