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I'll 1201 <br /> Subsurface Investigation ResuEts <br /> 6131 Pacific Ave., Stockton, CA. <br /> Aegis Project 4Io. 90-020 <br /> Page 7 <br /> 2.45 UTILITrES <br /> Prior to beginning any field. work, Underground Service Alert <br /> (USA) was be contacted and all underground utilities marked. <br /> Additionally, to prevent drilling through subsurface utilities, <br /> the first five feet of all borings were advanced by hand auguring <br /> techniques. <br /> 2.6.1 On-S3te U der ound Fti hies <br /> Underground utilities that service the Site include water, <br /> electric sanitary and storm sewer. Locations of the underground <br /> utilities are shown on Figure 4. Electric service is accessed <br /> from the western border of the Site by overhead wires to a <br /> 11tility pole. Electric service is provided to the kiosk 'via <br /> underground conduit from this Utility <br /> hone <br /> exists on the western edge of the sie , and itPole. A tiseassumedooth that <br /> t <br /> the booth is serviced by underground conduit that run along the <br /> west side of the site. Telephone service in the kiosk is most <br /> likely serviced by underground cables that run from the booth to <br /> the station building. The water and sanitary sewer access .the <br /> property at the northeast corner of the Site from Porter Avenue. <br /> 2.6.2 Off-Site Utilities <br /> Approximate locations of water, sanitary sewer, and storm sewer <br /> lines beneath servicing the site are shown on Figura 4. The City <br /> Of Stockton maintains sanitary and storm sewers. Cal Water <br /> maintains the water service. Pacific Gas and Electric maintains <br /> the natural gas and electric service in the area. <br /> 2.7 SITE BUESURFACE CONDITIONS <br /> Surface geologic strata in the vicinity of the Site consist of <br /> undifferentiated recent basin alluvium and units in the Victor <br /> Formation (DWR, 1967) . The strata were deposited in alluvial fan <br /> 'l and flood plain environments, and include lenticular gravel, <br /> sand, silt, and clay. The age of these deposits ranges from <br /> Pleistocene to Holocene. In the vicinity of the site these <br /> ` deposits are approximately 70 feet deep below grade. <br />