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bond <br /> Sierra Nevada that interfinger with the poorly sorted clays and silts of the Coastal Ranges. <br /> Cretaceous and Tertiary strata contain laterally continuous beds of mudstone, siltstone, <br /> conglomerate, sandstone, and limestone. Quaternary to recent units consist of lake and alluvium <br /> deposits. Soil encountered beneath the site generally consists of interbedded fine grained sand <br /> and clay with silty sand and sand from ground surface to the total explored depth of approximately <br /> 115 feet below grade (fbg). The interbedded layers range in thickness from approximately 5 to 20 <br /> feet thick. <br /> 2.3 Regional and Site Hydrogeology <br /> The site lies within the Eastern San Joaquin Groundwater Basin. The basin is bound to the north by <br /> the Mokelumne River, to the west by the San Joaquin River, to the south by the Stanislaus River, <br /> and to the east by consolidated bedrock. The nearest major surface water body is Yosemite Lake, <br /> approximately 3,500 feet to the west of the site. Groundwater flow within the basin is dominated by <br /> a large cone of depression located east of Stockton due to agricultural pumping. Wells at the site <br /> have been installed in four water-bearing zones. The shallow A Zone extends from approximately <br /> 30 to 45 fbg, the B' and B Zones extend from approximately 55 to 70 fbg and 75 to 85 fbg, <br /> respectively, and the C Zone extends from approximately 100 to 120 fbg. The aquitards between <br /> each water-bearing zone primarily consist of silts, which allow some hydraulic communication <br /> between the water-bearing sand zones. <br /> 2.4 Environmental History <br /> In 1999, three 10,000-gallon capacity underground storage tanks (USTs) used for gasoline and <br /> diesel fuel were removed from the site. The UST pit area was over-excavated with excavation <br /> dimensions of approximately 35 feet by 40 feet by 15 feet deep (Stantec Consulting Corporation <br /> [Stantec] 2011). During the excavation of the impacted soil, unidentified fiberglass piping was <br /> discovered (Stantec 2011). Additional excavation work and sampling were completed on April 8, <br /> 1999 to remove the unidentified piping. <br /> A brief overview of environmental assessment and remediation activities conducted at the site are <br /> presented below and more details for each assessment and remediation event are presented in <br /> Attachment B. <br /> 2.4.1 Previous Environmental Assessment <br /> Previous environmental activities at the site include the installation of twenty-three groundwater <br /> monitoring wells, six remediation wells, eight soil borings, and six soil vapor probes. Four of the six <br /> soil vapor probes were temporary and were destroyed after they were sampled. <br /> 2.4.2 Previous Environmental Remediation <br /> Remedial activities at the site began in 1999 with the removal of all site infrastructure, including <br /> USTs, dispenser islands and product piping, and over-excavating hydrocarbon-impacted soil <br /> (approximately 1,707 tons) in the vicinity of the USTs and dispenser islands. From March 2010 to <br /> June 2012, mobile oxygen injection events were conducted every two weeks and reportedly <br /> GHD I Well Installation Work Plan Addendum 111193145(5)1 Page 2 <br />