When the local stresses along the fault become too large, the fault slips suddenly or ruptures and releases the stored strain energy. ... When a rupture occurs along a fault, the strain energy stored on either side of the fault is released in the form of seismic waves and heat.
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When the local stresses along the fault become too large, the fault slips suddenly or ruptures and releases the stored strain energy. ... When a rupture occurs along a fault, the strain energy stored on either side of the fault is released in the form of seismic waves and heat.
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