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I <br /> 1 <br /> • Site Background Information <br />' QUICK N SAVE#2 <br /> 2057 South El Dorado Street,Stockton, California <br />' <br /> INTRODUCTION <br />' The site is located on the west side of South El Dorado Street and is bounded on the north by Delhi <br /> Street,in an area of low topographic relief at an elevation of approximately 10 feet above mean sea <br /> level in the City of Stockton, California(Figure 1) The surrounding area is utilized for residential <br /> and light commercial purposes Currently the site is being utilized as a gasoline refueling station and <br /> mini mart <br /> t <br /> REGIONAL GEOLOGIC/HYDROLOGIC SETTING <br />' The property is situated within the Great Valley Geomorphic Province of California, a large, <br /> elongate, northwest trending, asymmetric structural trough The Great Valley Province has been <br />' filled with thick sequences of sediment ranging in age from Jurassic to Recent,creating a nearly flat- <br /> lying alluvial plain that extends from the Tehachapi Mountains in the south to the Klamath <br /> Mountains in the north The western and eastern boundaries of this province are comprised of the <br />' • Cahfornia Coast Range and the Sierra Nevada, respectively Rocks composing the basement <br /> complex of the province have not been completely defined but are believed to be metamorphic and <br /> igneous in origin The northern and southern portions of the Great Valley Province have been <br />' designated the Sacramento and San Joaquin Valleys, respectively <br /> Based on the General Soil Map from the San Joaquin County Soil Survey,published by the United <br /> States Department of Agriculture Soil Conservation Service in 1992, the site area is within the <br /> Jackson-Hallenbeck-Stockton (JHS) association The JHS soils are located within basins, and <br /> generally consist ofrnoderately-to poorly-drained,fine-textured soils The soils are generally derived <br /> from both marine and non-marine sediment, and are typically formed in alluvium derived from <br />' mixed rock sources <br /> The Modesto, Riverbank, and Turlock Lake Formations and overlying Recent alluvium are the <br /> principal source 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 />' The closest surface water features to the site are the San Joaquin River and Walker Slough, located <br /> approximately 4,500 feet southwest of the site Water from the site drams into the San Joaquin River <br />' Deep Water Channel,which is primarily used for commercial and recreational boating Based upon <br /> well information obtained from the most recent quarterly monitoring event(August 2004), ground <br /> water flow direction is toward the east-southeast and is currently occurring at a depth of <br />' approximately 31 feet to 32 feet below surface grade(bsg) <br />' Advanced GeoEnvironmental,Ine. <br /> 1 <br />