Here's a breakdown:
* Strike: The strike of a fault is the direction of the line of intersection between the fault plane and a horizontal surface.
* Dip: The dip of a fault is the angle between the fault plane and the horizontal plane.
* Strike-slip Fault: In a strike-slip fault, the movement is primarily along the strike of the fault. This means the blocks of rock slide past each other horizontally.
There are two types of strike-slip faults:
* Right-lateral: When looking across the fault, the opposite side moves to the right.
* Left-lateral: When looking across the fault, the opposite side moves to the left.
Examples of strike-slip faults:
* San Andreas Fault (California): A right-lateral strike-slip fault responsible for major earthquakes.
* North Anatolian Fault (Turkey): A right-lateral strike-slip fault responsible for numerous earthquakes.
Let me know if you have any other questions!