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27 December 1996 <br /> AGE-NC Project No 95-0143 <br />' Page 2 of 19 <br /> 23 REGIONAL GEOLOGICAL/HYDROGEOLOGICAL SETTING <br />' <br /> The site is situated within the Great Valley Geomorphic Province of California, a Iarge, elongate <br /> northwest tending, asymmetric structural trough The Great Valley Province has been filled with <br /> thick sequences of sediment ranging in age from Jurassic to Recent, creating a nearly flat Iying <br /> alluvial plain, which extends from the Tehachapi Mountains in the south to the Klamath Mountains <br />' in the north The western and eastern boundaries of this province are comprised of the California <br /> Coast Range and the Sierra Nevada, respectively Rocks composing the basement complex of the <br /> province have not been completely defined but are believed to be of metamorphic and igneous <br />' origin The Great Valley Province has been subdivided into two major divisions identified as the <br /> Sacramento and San Joaquin Valleys <br />' The Modesto Riverbank and Turlock Lake Forn-iations and overlying Recent alluvium are the <br /> principal sources of domestic ground water in the 13,500-square mile San Joaquin Valley Ground <br /> Water Basin (Basin 5-22) This basin is drained primarily by the San Joaquin River <br /> 1 <br /> 2 4 LOCAL GROUND WATER SETTING <br /> The closest surface water feature to the: site is the Stockton Deep Water Channel (McLeod Lalte) <br />' located approximately 500 feet south of the site Water from the Deep Water Channel is ptimarily <br /> used for commercial and recreational boating Ground water is currently encountered at a depth of <br /> approximately 21 feet below surface grade (bsg), and has a northerly flow direction, away from the <br />' deep water channel Since the Deep Water Channel is up-gradient with respect to the ground water <br /> flow direction, impacted water at the site does not pose a threat to beneficial use of the Deep Water <br /> Channel Ground water occurs in a generally sandy Iayer extending from approximately 20 feet bsg <br />' to 36 feet bsg The sedimentary units are relatively horizontal and continuous over the site Recent <br /> depth to ground water information is summarized on Table 2 <br /> 25 MUNICIPAL WELL SURVEY <br /> Drinking water near the site is supplied by the City of Stockton municipal wells California Water <br /> Service Company (Cal Water) maintains a municipal well and tank approximately 1,100 feet west <br /> I of the site at Lindsey Street and Edison Street No other municipal wells maintained by the City of <br /> Stockton or Cal Water are located within 2,000 feet of the site The nearest municipal well located <br /> down-gradient from the site is approximately 2,600 feet northeast of the site on East Poplar Street, <br /> between San Joaquin Street and Hunter Street First encountered ground water is not used for <br /> drinking or irrigation <br /> I <br />