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Site Background Information <br /> I FORMER FISCO WAREHOUSE (Howard Lenz Property) <br /> 1648 Shaw Road, Stockton, California <br /> The site is located in a commercial area of low topographic relief in east Stockton, California, at an <br /> Iapproximate elevation of 25 feet above mean sea Ievel The site is bounded on the north and east by <br /> the Stockton Diverting Channel,on the west by State Highway 99 and on the south by Shaw Road <br /> Golden West Irrigation,an agricultural irrigation supply and distributing facility,presently occupies <br /> the property <br /> REGIONAL GEOLOGIC/HYDROGEOLOGIC 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,extending 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 /> I province have not been completely defined but are believed to be metamorphic and igneous origin <br /> The northern and southern portions of the Great Valley Province have been designated the <br /> Sacramento and San Joaquin Valleys,respectively <br /> The Modesto,Riverbank,Turlock Lake Formations and overlying recent alluvium are the principal <br /> source of domestic ground waterin 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 300 feet <br /> north of the site The Stockton Diverting Canal usually contains little water and has not appeared to <br /> have a significant effect upon ground water depth or flow direction in the area, however the canal <br /> could be the cause of the significant fluctuation in ground water flow direction and depth at the site <br /> HYDROGEOLOGICAL MODEL <br /> Based on the CPT results, AGE has developed a preliminary subsurface model of the site soil <br /> stratigraphy comprised of four informal zones, a vadose (unsaturated) zone and three hydrological <br /> I units Hydrological units may be defined as significant vertical intervals of soil having significant <br /> lateral extent and having sinular hydrologic characteristics (i e hydraulic conductivity, <br /> transmissivity, etc ) over its vertical and horizontal extent A `flow unit' may be defined as a <br /> I hydrologic unit and is characterized by significantly greater hydraulic conductivity values than <br /> overlying and underlying units A flow umt is capable of serving as a preferred migration route, and <br /> could potentially allow migration of large contaminant masses over great distances <br /> IAdvanced GeoEnviren mental,Inc <br /> I <br />