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4) Total length from Witkind (1976) or Kirkham and Rogers (1981}. <br />5) Rupture length estimated from pattern of mapped traces of seismogenic sources. <br />6) Rupture width based on estimated crustal thickness (20 km), dip of fault, and focal depths of historical seismicity. <br />7) Rupture area is the product of rupture width and rupture length. <br />8) Slip rate based on, and calculated from the fault activity data in Butler and Nicholl (1985), the age of displacement data in <br />Kirkham and Rogers (1981), and the rupture versus magnitude relationships of Wells and Coppersmith (1994). <br />9) The MCE (maximum credible earthquake) is a moment magnitude (Mw) that was calculated using the fault rupture versus <br />earthquake magnitude relationships of Wells and Coppersmith (1994), and the individual geologidgeometric data for each <br />potential seismogenic source. <br /> <br /> <br />Golder Associates <br />