High-resolution surface faulting from the 1983 Idaho Lost River Fault M_w 6.9 earthquake and previous events.

The frequency graph of the synthetic Qfs shows a wider distribution of the values between 1.5 and 4.5 m, with a peak between 3 and 3.5 m and a median value of ~3 m; the frequency graph of the antithetic faults shows a peak correspondingt to 50 cm and a median of about 1 m in a decreasing trend up to 5.5 m.

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