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A fault is a crack or fracture in Earth's crust caused by the movement of landmasses, called plates, on either side of the fault line. Faults are found either at the surface (fault surface) or underground (fault plane). Most earthquakes occur along fault lines. The principle types of faults are: normal, reverse, thrust, and slip-strike.

Normal faults form when two plates are under tension and are being pulled or stretched apart. When this occurs, Earth's crust thins and one plate rises or drops against the other. More than 200 million years ago, North America and Africa were one huge landmass. Plates on either side of a massive fault line ruptured and began drifting apart. Oceanic waters, now known as the Atlantic Ocean, surged into the valley between, and two separate continents were born.

In contrast, reverse faults form from compression: two plates are being pushed into one another. The compression forces one plate up...