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Inland earthquakes which produced by slip on active faults have recurrence times of more than thousand of years. Historical records of destructive earthquakes is insufficient to characterize the seismicity. Assessment of the seismic potential of an active fault is therefore often difficult. Only geological and geomorphological methods enable to estimate the recurrence times. Analyses of the stratigraphy and Carbon-14 ages of the two boreholes which arranged close to a fault have revealed the last two earthquakes produced by the fault in this study. The last earthquake occurred after 2,500 years before present (yBP), and the penultimate one occurred between 5,300yBP and 4,300yBP. The last one is likely to be correlated with the historical earthquake of 850 A.D.. 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