Normal faults experience tensional stress while strike-slip faults involve lateral movement along the fault line.
A normal fault is under tension. In a normal fault, the hanging wall moves down relative to the footwall due to tensional stress. It is created by tensional forces in the Earth's crust and often occurs at divergent plate boundaries.
On the other hand, strike-slip faults exhibit side-to-side motion without vertical displacement. They are commonly associated with transform plate boundaries and are prevalent in transform fracture zones along mid-ocean ridges.
Therefore, in the context of faults, normal faults experience tensional stress, while strike-slip faults involve lateral movement along the fault line.
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