Failed rifts remain as zones of weakness that may be reactivated by later plate-tectonic stresses to once again generate earthquakes.

Question

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Failed rifts represent areas of weakened crust that can be reactivated by tectonic stresses, leading to the formation of new faults and potential earthquakes. Therefore, failed rifts can be considered as zones of weakness that are susceptible to seismic activity in the future.

Failed Rifts Remain as Zones of Weakness That May Be