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r Clayton <br /> ,N1RONWNTm <br /> CO,NSLfLTANT5 <br /> Quaternary (recent) San Joaquin Formation alluvium according to the California <br /> Department of Conservation, Division of Mines and Geology. <br /> According to the USGS Manteca, California, 7-1/2 minute topographic quadrangle <br /> map, the elevation of the site is approximately 3 feet above mean sea level. The <br /> regional topographic slope trends to the northwe terly parallel with the San Joaquin <br /> River. Regional surface drainage would tend to follow the slope. <br /> Based on California Division of Oil and Gas maps, the site is not located within an oil <br /> or gas field. <br /> Based on information from the Water District, the depth to groundwater under the <br /> subject site is approximately 30 to 35 feet and g oundwater flow direction is <br /> northwesterly. However, the site is over an area that is actively pumped for irrigation <br /> water and the groundwater flow direction may vary. <br /> No known faults transect the site. In addition, the area is not located within a fault- <br /> rupture hazard zone as defined by the 1972, State of California Alquist-Priolo Special <br /> Studies Zones Act. However, the site is surrounded by fault zones and could be <br /> subject to ground motion during earthquakes associated with these faults. <br /> According to the City of Manteca, records indicate that this site is not located within <br /> a 100- or 500-year flood zone and is, therefore, not in an area that has a potential for <br /> flooding. <br /> 4.1 FIELD RESULTS <br /> The soil encountered was a fine- to medium-g ed sand from the surface to a depth <br /> of approximately 8 feet below grade. At this de th, clayey silt was encountered <br /> which continued to the maximum depth of the tree boreholes. Groundwater was not <br /> encountered at the maximum depth of 10 feet be ow grade. <br /> The PHYremeasured 0 to 1.8 parts per million (ppm) on the soil samples collected from <br /> the boreholes (Appendix Q. The low-level readings on the PID are likely <br /> interference associated with the high moisture c ntent in the samples, not with YOC <br /> vapors. During the drilling and sampling, Clayt n did not detect any fuel-like or <br /> chemical-like odors or staining. <br /> 4.2 LABORATORY RESULTS <br /> The laboratory reported no detection of gasoline benzene, toluene, ethylbenzene, and <br /> xylenes (BTEX), or organic Iead in any of the soil samples, at the laboratory <br /> detection limits specified in the laboratory reports (Appendix D). A summary of <br /> laboratory results are included in Table 1 (Appendix A). <br /> 4 <br /> 4014.00.REP CO FIDENTIAL AND PRIVILEGED <br />