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&Anurface 1n _ tigatlm Resotte <br /> 4.131 Va^ffic Ave., Stockton, eA. <br /> Ae91e Project No. 90-020 <br /> Page 9 <br /> i <br /> A TE IdXAAOOEOL4GIC/ REGIONAL GEOLOGY <br /> A complete review of the is included in Aegis' Pre-Tank <br /> Replacement Site Assessment Work Plan (Aegis March 6, 1990) . <br /> 2.9 WATER WELL I*:FORMATION <br /> A water well search will be conducted through the State of <br /> ca-iifornia Department of Water Resource.^, to located water wells <br /> _'_thin 1/2 mile radius of the Site. <br /> 3.0 RESULTS OF SUBSURFACE INVESTIGATION <br /> A total of fourteen soil borings were advanced at the locations <br /> shewr. on Figure B. Soil borings B-9 through B-14 were: advanced to <br /> 1.. 0 feet below grade. Soil borings B-2 through B-8 were advanced <br /> 46.0 feet below grade, soil boring B-1 was drilled to 55 feet <br /> below grade. Logs of the soil borings are included in Appendix B. <br /> A total of 28 soil samples from the borings were submittel to a <br /> state-certified-laboratory for analyses. Copies of laboratory ; <br /> reports are included in Appendix C. <br /> 3.1 SOIL CONDITIONS <br /> Fourteen soil borings were drilled, sampled and logged, ac�ording <br /> to the methods described in Appendix A (B-1 was not samples) . The <br /> soil borings ranged from 21.0 ft. to 55 ft. below grade. Sail <br /> Loring B-1 was advanced to ground water, away from suspected soil <br /> contamination. <br /> Ine soil boring logs were used to compile generalized cro= <br /> sec,-.ion A-A, ' which is presented in Figure 6. As depicted -In the <br /> -- cross section, silts varying--fromclayey. to scndy composition <br /> were the predominant soil type encountered (unified Soil <br /> Classification System symbol ML) . Generally silty clays occurred <br /> at shallow depths, followed by interlayered horizons of sa::%dy <br /> silts. Most of the deeper borings ended in clayey silts. Soil <br /> types ranged from a fine grained silty clays to medium grained <br /> silty sand, to sand. As shown on the cross section, soil type- <br /> '- beneath the site generally coarsen with depth. <br />