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generate large earthquake loads at the Forward Landfill. An MPE moment <br /> magnitude (Mw) 6.4 earthquake on the Great Valley fault would generate a <br /> PGHA of approximately 0.098; an MCE MW 6.7 event on the Great Valley fault <br /> would generate a PHGA of approximately 0.13g. <br /> While the Great Valley fault was calculated to yield the highest PHGA, the <br /> duration of earthquake-induced ground shaking would be longest for the San <br /> Andreas fault system. The MPE and MCE on the San Andreas fault system are <br /> characterized by the same MW 7.9 event at a distance of 70 miles (112 km). As <br /> shown on Table 4, such a large-magnitude distant event is calculated to induce <br /> strong ground shaking that could last 45.4 seconds. Given the relatively small <br /> difference in the estimated bedrock PHGA and the relatively large difference in <br /> estimated Dy Geosyntec concluded that the M,v 7.9 event on the San Andreas <br /> fault system could be the most damaging earthquake for the Forward Landfill. <br /> Accordingly, the MW 7.9 event on the San Andreas fault system should be <br /> considered for evaluation of both MPE and MCE design ground motions at the <br /> Forward Landfill along with the appropriate M,,event on the Great Valley blind <br /> thrust system. <br /> A target acceleration response spectral envelope was developed by Geosyntec <br /> for each of the MCE/MPE candidate events using the median and 84" percentile <br /> acceleration response spectra evaluated using the Abrahamson and Silva [19971 <br /> attenuation model. Based upon the target significant duration of strong ground <br /> shaking and acceleration response spectral envelope for each candidate event, <br /> the following four time histories were selected to represent potential ground <br /> motions at a hypothetical bedrock outcrop at the site: <br /> • the 270-degree component of the Saratoga-Aloha Avenue record from the <br /> M,, 6.9 Loma Prieta earthquake, scaled to either 0.19 g to represent the MCE <br /> or to 0.13 g to represent the MPE; <br /> • the 315-degree component of the Santa Teresa Hills record from the MW 6.9 <br /> Loma Prieta earthquake, scaled to either 0.19 g to represent the MCE or to <br /> 0.13 g to represent the MPE; <br /> • the 360-degree component of the Corralitos-Eureka Canyon Road record <br /> from the MW 6.9 Loma Prieta earthquake, scaled to either 0.19 g to represent <br /> the MCE or to 0.13 g to represent the MPE; and <br /> Forward Landfill)TD 3-6 <br /> L:\Allied\2000.193\Reports\jtd:Sec-3.0:05/21/02 <br /> BRYAN A.BTIRRAT&.ASSOCIATES <br />