Laserfiche WebLink
1 <br /> 29 March 2004 <br /> i AGE-NC Project No. 97-0327 <br /> Page 2of12 <br /> ' The site presently consists of two 12,000-gallon gasoline/diesel USTs, one mini-market building, <br /> one carwash building and fuel dispensing islands under a canopied structure. <br /> The site is currently connected to the City of Stockton sanitary sewer system,which is located along <br /> ' the easement in the west section of the property along Oro Avenue. It is AGE's understanding that <br /> no septic tank has been utilized on the property since 1966. <br /> 2.2. REGIONAL GEOLOGIC/HYDROGEOLOGIC SETTING <br /> The property is situated within the Great Valley Geomorphic Province of California, a large, <br /> elongate, north-northwest trending, asymmetric structural trough. The Great Valley Province has <br /> t been filled with thick sequences of sediment ranging in age from Jurassic to Recent,creating a nearly <br /> flat-lying alluvial plain, extending 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 />' California 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 of moderate to poorly drained fine textured,soils. The soils are generally derived <br /> from both marine and non-marine sediment, and are generally formed in alluvium derived from <br /> mixed rock sources. <br />' The Modesto,Riverbank,Turlock Lake Formations and overlying recent alluvium are the principal <br /> source of domestic ground water in the 13,500 square-mile San Joaquin Valley Ground Water Basin <br />' (Basin 5-22). This basin is drained primarily by the San Joaquin River. The nearest surface water <br /> feature in the vicinity of the property is the Stockton Diverting Canal located approximately 2,500 <br /> feet north of the site. <br />' Based on regional information from Lines Of Equal Depth To Ground Water and Lines of Equal <br /> Elevation Of Ground Water, published by the San Joaquin County Flood Control and Water <br /> Conservation District between 1971 and present, the depth to ground water at the:property has. <br /> generally fluctuated between 50 and 80 feet bsg;regional ground water flow direction has generally <br /> been oriented towards the northeast. <br />