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Field and excavation investigations show that at least two paleo­ (historic) seismic events occurred along the northeastern segment of the Chelungpu fault during the period between 1800 AD and 500 AD before the 1999 Chi-Chi earthquake. The principal indicators of paleo-seismic faulting events are: (i) termination of secondary faults, (ii) deformation of deposits related to faulting, and (iii) liquefaction of deposits. The observa­ tional results show that the offset produced by an individual faulting event is 1 m. It is inferred that the probable magnitude of these two paleo­ earthquakes is 7.0-7.5. (

Geological Evidence of Paleo-seismic Events Occurred along the Chelungpu Fault Zone, Taiwan