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Site Characterization:Clover li�dle School,51 East Beverly Place, Tracy, CA. Page 3 <br /> are of Quaternary to Recent age. The soils are dominantly silty and sandy clays <br /> with interbeds of silt, sand and gravel. The general direction of groundwater <br /> flow in the neighborhood is to the north towards the Old River anatomic <br /> branch of the San Joaquin River and its tributaries that include Tom Paine <br /> Slough and Sugar Cut. <br /> �. The depth to groundwater in the central Tracy area is typically 7 to 10 ft. It <br /> varies seasonally with at its highest elevation usually occurring in February and <br /> its lowest in September. Mean groundwater elevations in the area have been <br /> �w slowly dropping over the last 20 years. Groundwater gradients are typically <br /> 0.003 ft./ft to the north or north-northwest. <br /> 2.1 Search for Existing Wells <br /> An initial search for the presence of existing off-site agricultural, industrial, <br /> AW domestic, municipal and other wells within a 2,000•ft. radius of 51 East <br /> Beverly Place was made using United States Geological Survey (USGS) <br /> topographical maps and the searchable electronic databases available from <br /> Vista Information Solutions, Inc. (Vista) of San Diego,California. <br /> No wells within a radius of 2,000 feet of the subject property are shown on the <br /> USGS 7.5' series maps of the Union Island and Tracy Quadrangles. <br /> The Vista searchable electronic database contains information from 25 Federal <br /> and State regulatory agency databases, as well as the Federal Reporting Data <br /> System (FRDS), which provides information on wells that are used by 194,000 <br /> communities and water-supply systems. A search of the Vista database yielded <br /> 46 citations to well sites in the 95376 Zip Code, which includes the Tracy area. <br /> The list of wells found by the search is presented in Appendix B. It was <br /> possible to eliminate all of the listed sites from consideration with respect to <br /> " the Alfred Clover Middle School property because they are located in excess of <br /> 2,000 feet from that property. <br /> Although no wells within 2000 f1 of the subject property were found by the <br /> electronic search of government databases, it is SJC's experience from working <br /> in Tracy and similar communities in the Central Valley of California,that those <br /> databases frequently do not include a number of domestic or agricultural water <br /> supply wells that may be present in a area, particularly if the wells are no <br /> longer used or have been abandoned. Accordingly, SJC staff made a tour of the <br /> school grounds and the neighboring area to search for wells that may not have <br /> been recorded in the databases. The search located a deep water supply well on <br /> the school grounds just over 100 ft to the west, and co-gradient from, the <br /> former site of the underground fuel storage tank. <br /> The location of the well described above is shown on Figure 2. No well log has <br /> been found, but the well appears to have been designed to draw water from an <br /> SJC <br />