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14 April 2004 <br /> AGE-NC Project No.04-1143 <br /> Page 2 of 17 <br /> /3.0. REGIONAL GEOLOGIC/HYDROGEOLOGIC SETTING <br /> The subject 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 to its present elevation with thick sequences of sediment ranging in age from Jurassic to <br /> Recent, creating a nearly horizontal alluvial plain, extending from the Tehachapi Mountains in the <br /> south to the Klamath Mountains in the north. The western and eastern boundaries of this province <br /> are comprised of the California Coast Range and the Sierra Nevada,respectively.Rocks composing <br /> the basement complex of the province have not been completely defined but are believed to be <br /> metamorphic and igneous in origin.The northern and southern portions of the Great Valley Province <br /> have been designated the Sacramento and San Joaquin Valleys, respectively. <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. The nearest <br /> surface water feature was the East Bay Municipal Utility District(E.B.M.U.D)Mokelume Aqueduct <br /> approximately 200 feet towards the southeast. <br /> As included in the report prepared by Environmental Data Research, Inc. (EDR) and provided in <br /> '- Appendix D of this report, the U. S. Department of Agriculture's Soil Conservation Service <br /> STATSGO (State Soil Geographic Database) soil maps showed the dominant soil composition in <br /> the general area of the subject property to be CLEAR LAKE soil,a clay in a Class D Hydrogeologic <br /> Group, which includes very slow infiltration rates. The corrosion potential for uncoated steel was <br /> high. <br /> The estimated depth to ground water at the subject property is approximately 100 feet below surface <br /> grade(bsg),based on the map titled Lines of Equal Depth to Groundwater, Spring 1999 published <br /> by the San Joaquin County Flood Control District and Water Conservation District(FCD&WCD). <br /> It is inferred from the map titled Lines of Equal Elevation of Groundwater, Spring 1999, also <br /> published by the FCD&WCD, that the local ground water flow is indeterminate at the subject <br /> property and in an area of ground water lows; this may be greatly modified by local recharge and <br /> discharge patterns. Ground water is considered to be of beneficial use and is utilized for domestic, <br /> industrial and commercial purposes. <br /> 1� 4.0. HISTORICAL USE <br /> The history of the subject site from as early as 1957 to present was researched by reviewing aerial <br /> photographs, topographic maps, directory listings, Pesticide Use reports and a personal interview. <br /> ... Advanced GeoEnvironmental,Inc. <br />