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EARTH'S CRUST
Faults are fractures in Earth’s crust where movement has happened. Occasionally faults move when energy is released from a unexpected slip of the rocks on either side. Most earthquakes happen along plate boundaries, but they can also occur in the middle of plates along intraplate fault zones.
Some faults can be seen at the surface, but others lie deep within the crust. Just as there are different types of plate movements, there are also different types of faults. They ’re based on the type of movement they show.
Normal faults are frequently establish along divergent plate boundaries, similar as under the ocean where new crust is forming. Long, deep valleys can also be the result of normal faulting.
Reverse fault produce when the rocks on the “ uphill” side of an inclined fault plane rise above the rocks on the other side.
Strike-slip Faults Occasionally related to as a lateral fault, this kind forms when the blocks of rock on either side of a vertical.
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