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I - <br />' SITE BACKGROUND INFORMATION <br /> STRONG PROPERTY <br />' 5157 West Business Loop 205, Tracy, California <br />' The site is located on the north side of West Business Loop 205 between Bird Road and Banta Road, <br /> approximately three miles east of Tracy, San Joaquin County, California (Figure 1). The site is <br /> located within the southeast quarter of Section 24, Township 2 South,Range 5 East,Mount Diablo <br />' Base and Meridian (Vernalis Quadrangle, 7.5-Minute USGS Topographic Series, 1991). <br />' One structure is located on the property and is presently unoccupied. It is our understanding that the <br /> site historically operated as a truck depot. <br />' REGIONAL GEOLOGIC SETTING <br />' According to Geologic Map of California (1966, California Department of Conservation Division <br /> of Mines and Geology), the site area is within the Great Valley Geomorphic Province (GVGP) of <br /> California, a large,elongate,northwest trending structural trough.The GVGP is subdivided into two <br />' major divisions designated the Sacramento.and San Joaquin Valleys, which have been filled to the <br /> present elevation with thick sequences of sediment ranging in age from Jurassic to present day, <br /> creating a nearly flat-lying alluvial plain extending from the Tehachapi Mountains in the south to <br />' the Klamath Mountains in the north. The western and eastern boundaries of this province are <br /> comprised of the California Coast Range and the Sierra Nevada, respectively. <br />' Based on General Soil Map (1992, United States Department of Agriculture Soil Conservation <br /> Service) obtained from the San Joaquin County Soil Survey, the site area is shown as being within <br /> the Capay-Stomar-Zacharias(CSZ)soil association.The CSZ soils are located on interfan basins and <br />' on alluvial fans and stream terraces in the southwestern part of San Joaquin County. The soils <br /> generally consist of moderate to well drained, fine textured soils. The CSZ soils generally formed <br />' in alluvium derived from sedimentary and mixed rock sources. <br />' GROUND WATER DEPTH AND GRADIENT - REGIONAL <br /> Based on information from the Lines Of Equal Elevation Of Water In Wells - Unconfined Aquifer <br />' Spring 1993, published by the California Department of Water Resources, the estimated ground <br /> water elevation at the site is approximately 50 feet above sea level. Based on an approximate <br /> elevation of 35 feet above sea level, the depth to ground water at the site is assumed to be 15 feet <br />' below surface grade (bsg). The regional ground water flow direction near the site area is generally <br /> toward the north, although flow directions may vary locally and seasonably. <br /> I <br />' Advanced GeoEnviromnental,Inc. <br />