How will you describe the movement of the walls in a strike slip fault?

Question: How will you describe the movement of the walls in a strike slip fault?

In a strike-slip fault, the movement of the walls is primarily horizontal, with the two blocks of crust sliding past each other along the fault line. This movement can be either right-lateral (dextral), where the opposite block moves to the right, or left-lateral (sinistral), where the opposite block moves to the left. The motion is driven by shear stress acting parallel to the fault plane, often resulting in significant earthquake activity due to the build-up and release of stress. A well-known example of a strike-slip fault is the San Andreas Fault in California.

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