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There are several types of stresses that can cause earthquakes, including tension, shearing, and compression. Tension occurs when rocks are pulled apart, shearing when rocks slip past each other, and compression when rocks are squeezed together. Normal faults are caused by tension in the earth's crust and form when the hanging wall above the fault is pulled away from the footwall below. Compression stress can squeeze and fold rocks, contributing to the formation of mountains.






