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1* <br />4.5 Site and Area Lithology *,y <br />According to BC, the subject site is located in the San Joaquin Valley which is a north -south trending�.j�' ha <br />basin bounded by the Sierra Nevada Mountain Range to the east and the Coast Ranges to the West' <br />`� <br />Within the Stockton area the valley floor consists of Quaternary age alluvial sediments deposited by the01 ,`r�� <br />San Joaquin River and its tributaries Soil hthology in the Stockton area includes sands, silty sands, silts, ` <br />clayey silts and clays <br />The site lies at an elevation of approximately 25 feet above mean sea level Sediment deposition in the <br />area has produced nearly horizontal topographic features in the vicinity of the site Soils encountered <br />beneath the site during the previous assessment activities consist of inter -bedded alluvial deposits, <br />including clays, silts, sands, and fine gravels <br />4.6 Area Hydrology and Hydrogeology <br />According to BC, the San Joaquin River is the major surface drainage within the Stockton area of the San <br />Joaquin Valley The river flows approximately 40 miles from its point of origin, in the central San <br />Joaquin Valley to Suisun Bay Groundwater in the valley flows west, from the Sierra Nevada Mountain <br />range, - fnd mast rcm- the Coastal :angcs, toYaaid,, the ec itei of the dailf'y, a,-11 tL O'1_1L°Tll <br />Valley Delta area The general groundwater flow direction in the Stockton area is reportedly to the <br />northwest, towards the Stockton Divertion Channel, and exists at approximately 50 to 100 feet bgs <br />Shallow groundwater is considered unconfined and has been designated as a beneficial water use unit <br />Groundwater is used for farming and ranching (irrigation of crops and watering of farm animals), <br />municipal and industrial water supply, and as a drinking water supply for the general public <br />The San Joaquin River is located approximately 4 miles southwest of the site However, the nearest body <br />of surface water, a water transportation and irrigation canal, is located approximately 3/2 mile northeast of <br />the site Within the last 10 years groundwater beneath the site has risen from approximately 80 to 50 feet <br />bgs. <br />5.0 RECENT SITE CHARACTERIZATIONS <br />In accordance with the ATC Workplan For Additional Assessment, dated December 21, 2001, ATC <br />installed five groundwater monitor wells (MW -13 through MW -17), three dual completion vapor <br />extraction/air sparge wells (VEAS-1 through VEAS-3), and one groundwater extraction well (EX -1) on- <br />site for the purposes of additional assessment and conducting pilot study activities The wells were drilled <br />and installed from December 9 through 20, 2002 The installation and assessment associated with the <br />drilling of groundwater monitor wells MW -13 through MW -17, remediation wells VEAS-1 through <br />VEAS-3, and groundwater extraction well EX -1 was presented in the ATC Additional Site Assessment <br />Report dated February 12, 2003 The ATC workplan was approved by Mr Harlan Knoll of the San <br />Joaquin County Public Health Services, in a letter received by ATC on May 22, 2002 A copy of the <br />approval letter is included as Appendix A — Regulatory Correspondence Appendix B outlines Standard <br />EZ 100966 CAP <br />S \EZ Serve\F-Z 1009661Reports1100966CAP <br />5 <br />ATC Associates Inc <br />ATC Project No 43 25827 0026 <br />