Answer:
C. SIDEWAYS
Explanation:
Vertical (or almost vertical) cracks where the blocks have primarily migrated horizontally are known as strike-slip faults. Right lateral motion occurs when the block opposite an observer gazing across the fault travels to the right; left lateral motion occurs when the block moves to the left. Strike-slip movement occurs when rocks on each side of a nearly vertical fault line move horizontally. An oblique-slip fault is a type of fault that occurs when movement is not parallel to the fault plane. Vertical (or almost vertical) cracks where the blocks have primarily migrated horizontally are known as strike-slip faults. Shearing forces cause the fault motion of a strike-slip fault. The fault is called left-lateral if the block on the far side of the fault slides to the left, as demonstrated in this animation.
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