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Lutzky Associates Development, LP - Geotechnical Investigation <br />MACTEC Projecl 4953-03-2631 <br />September 18.2003 <br />Tsunamis, Inundation, Seiches, and Flooding <br />The site is located about 7 miles from the Pacific Ocean at an elevation of approximately 42 feet <br />above mean sea level (U. S. Geological Survey datum). Therefore, tsunamis (seismic sea waves) <br />are not considered a significant hazard at the site. <br />According to the County of Orange Safety Element (1995), the site is not located downslope of <br />any large bodies of water that could adversely affect the site in the event of earthquake-induced <br />dam failures or seiches (wave oscillations in an enclosed or semi-enclosed body of water). <br />The site is not within the limits of a 100-year fiood zone or a 500-year flood zone, based on flood <br />maps published by FEMA (ESRUFEMA, 2003) <br />Subsidence <br />The site is not within an area of known subsidence associated with fiuid withdrawal (ground water <br />or petroleum), peat oxidation, or hydrocompaction (City of Santa Ana General Plan, 1982). <br />5.6 ESTIMATED PEAK GROUND ACCELERATION <br />Ground motions were postulated corresponding to the Design Basis EaMhquake (DBE), having a <br />10% probability of exceedence during a 50-year time period and the Upper Bound Earthquake <br />(UBE), having a 10% probability of exceedence during a 100-year time period. <br />The site-specific peak ground acceleration for the UBE was estimated by a Probabilistic Seismic <br />Hazard Analysis (PSHA) using the computer program EZFRISK, Version 5.71. The faults used in <br />the study are shown in Tables 1 and 2, along with the maximum magnitude and the slip rate <br />assigned to each fault. <br />The peak ground acceleration was estimated as the average of the ground motion attenuation <br />relations for a "soil" site classification discussed in Abrahamson and Silva (1997), Boore et al. <br />(1997), and Sadigh, et al. (1997). <br />14