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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 /> <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 /> <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