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v7nl, y, field prior to 1963. The whole site was an empty field in 1940. No other information regarding the site ownership or usage was available at the time of this report. Currently the property is occupied by two approximately 3,000 sq. foot, 1-story buildings; a cargo container; two scrap piles of metal and railroad timbers, respectively; asphalt parking areas; and soil and.vegetation on an approximately 4.9 acre lot. .The site boundaries are occupied by an eight-foot sheet metal fence. The two buildings consist of one cinder block building with a concrete slab floor, offices and service bays, located on W. Eleventh Street, and one wood framed building with corregated tin siding and a concrete slab floor located near the center of the site. In addition to the buildings on-site, there is a water supply well on the site, a septic tank and leach field located between the two buildings on-site, and a suspected hydraulic lift located north and adjacent to the cinder block building in a concrete slab. No underground storage tanks (USTs) are known to currently exist on the property. The property is provided water by the well on-site, and sewage is handled by the septic tank and leach field. Electricity and natural gas are provided by Pacific Gas and Electric Company. A generalized site plan is included as Figure 2. 3,3 Surrounding Land Uses Property along W. Eleventh Street in the vicinity of the site is comprised of commercial businesses, a truck refueling facility and light manufacturing. North and south of W. Eleventh Street and east of Chrisman Road land use is primarily agricultural. Immediately adjacent to the site to the east is a wooden truss manufacturing facility (Piedmont), to the north are railroad tracks, to the south is W. Eleventh Street, and to the west is a vacant lot with an abandoned house on it. The property across W. Eleventh Street from the subject site is a bar/club. 4.0 ENVIRONMENTAL SETTING 4_1 Regional Geologic Setting Tracy, California, is located in San Joaquin County and lies in the center of the large northwest trending asymmetrical structural trough called the Central Valley, adjacent to the Sierra-Nevada geomorphic provinces. The Central Valley contains a thick sequence of sediment which, in places, reaches a depth of 10 miles. These sediments range in geologic age from Jurassic (205 million years before present) to Recent (present time) and include both marine and continental deposits. wA9673 olph l rpt.doc 3