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Most earthquakes result from movements of the earth’s crust along faults. A fault is a fracture in the earth’s crust. The two sides of a fault move in different directions. These opposing movements set the stage for earthquakes to occur.
They cause the two sides of a fault to move past each other. Sometimes the rocks along the two sides of a fault may snag and remain locked. Tremendous stress builds in these areas as a the two sides of the fault attempt to move past each other.
The limit to how much stress a material can absorb is called its elastic limit: If you strech a rubber band too far, it will break and snap back...
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