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Escalon Subdivision <br /> Page 2 <br /> L May 30,2000 <br /> The site is located in Seismic Zone 3' and all structures should be designed accordingly. <br /> L There are no known faults that cross the site.The two closest active faults to the site are the Foothills <br /> Fault System located 20 miles east-northeast and the Great Valley Fault Zone located 24 miles west- <br /> southwest.','southwest',' Due to the relative proximity of these faults to the site there is a reasonable possibility <br /> that the site will be subjected to a moderate amount of shaking from a seismic event during the life <br /> of any structures. The California Division of Mines and Geology assigns a probabilistic (10% <br /> Lprobability of exceeding that motion in a 50 year period) peak horizontal ground acceleration for <br /> surface soil at the subject site of 0.1 to 0.2g.' A detailed analysis of earthquake induced liquefaction <br /> for the proposed site was outside the scope of our investigation,however the expected hazard is most <br /> L likely low due to the deep ground water, cohesive soils, and relatively lower earthquake induced <br /> ground motion for the area(0.1 to 0.2g). <br /> LFollowing is a table of the 1997 Uniform Building Code Soil Parameters'which may be used <br /> ii for design of structures at the subject site: <br /> 1997 UNIFORM BUILDING CODE SOIL DESIGN PARAMETERS <br /> Seismic Zone,Z 3 <br /> 1 L Soil Type,S Sd <br /> Seismic Source Type B <br /> Seismic Co-efficient,Ca 0.36 <br /> L Seismic Co-efficient,Cv 0.54 <br /> Distance to Foothill Fault Zone Source: 32 kilometers,20 miles <br /> Distance to Great Valley Fault Source: 39 kilometers,24 miles <br /> L <br /> The general topography of the site and surrounding area is relatively flat. At the time of our <br /> investigation,the site consisted of open agricultural fields with one house and barn.We understand <br /> that the field has undergone deep ripping (6 feet) of hardpan in two directions within the past 25 <br /> Lyears. <br /> ' Uniform Building Code, 1997 Edition,International Conference of Building Officials,Whittier,CA. <br /> L <br /> ' Blake,T.F., 1998a,A computer program for the probabilistic estimation of peak acceleration and utriform <br /> hazard spectra using 3-D faults as earthquake sources, IBM-PC and compatibles version, user's manual. Software <br /> update version 3.01 b, 1998. <br /> ' California Division of Mines and Geology, 1996,Probabilistic Seismic Hazard Assessment for the State of <br /> ` California, CDMG Open File Report 96-08. <br /> 4 ' California Division of Mines and Geology, 1999, Seismic Shaking Hazard Maps of California, CDMG <br /> LSeismic Shaking Hazard Map Sheet 48. <br /> O9L as. <br /> � ♦ 4 <br /> L <br /> O � <br /> ,da Off`, <br /> L <br />