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the Sierra Nevada, respectively. Rocks composing the basement complex of the province <br /> have not been completely defined but are believed to be metamorphic and igneous in <br /> origin. Northern and southern portions of the Great Valley Province have been <br /> designated the Sacramento and San Joaquin Valleys, respectively. <br /> The property and vicinity lie within the San Joaquin Valley Groundwater Basin, Eastern <br /> San Joaquin Subbasin (5-22.01). The Eastern San Joaquin Subbasin is defined by the <br /> areal extent of unconsolidated to semi-consolidated sedimentary deposits that are <br /> bounded by the Mokelumne River on the north and northwest; San Joaquin River on the <br /> west; Stanislaus River on the south; and consolidated bedrock on the east. The Eastern <br /> San Joaquin Subbasin is bounded on the south, southwest, and west by the Modesto, <br /> Delta-Mendota, and Tracy Subbasins, respectively and on the northwest and north by the <br /> Solano, South American, and Cosumnes Subbasins. The Solano and South American are <br /> subbasins of the Sacramento Valley Groundwater Basin. The Eastern San Joaquin <br /> Subbasin is drained by the San Joaquin River and several of its major tributaries namely, <br /> the Stanislaus, and Calaveras, and Mokelumne Rivers. The San Joaquin River flows <br /> northward into the Sacramento and San Joaquin Delta and discharges into the San <br /> Francisco Bay. <br /> Prevailing groundwater flow direction in Manteca generally ranges from north to <br /> northwest, but this may be greatly modified by local recharge and discharge patterns. <br /> Based on the map titled Lines of Equal Elevation of Groundwater Fall 2010, published by <br /> the San Joaquin Flood Control District and Water Conservation District (FCD&WCD), and <br /> on-going groundwater investigations in the area of the property (Regional Board's <br /> GeoTracker database), local groundwater flow is toward the north-northwest beneath the <br /> subject property. Based on the map entitled Lines of Equal Depth to Groundwater Fall <br /> 2010, also published by the FCD&WCD, and on-going groundwater investigations in the <br /> area of the property, depth to water is estimated at between approximately 15 feet and 20 <br /> feet below surface grade (bsg). Groundwater is considered to be of beneficial use and is <br /> utilized for domestic, industrial and commercial purposes. <br /> There are no surface water features on the property. The nearest surface water feature in <br /> the vicinity of the property is the San Joaquin River, which is located approximately 5 <br /> miles west of the property. <br /> The Phase I/RFA and Closure Report indicates that the Site is not located within either a <br /> 100-year or a 500-year Flood Zone. This data, available in select counties across the <br /> country, was obtained by EDR from the Federal Emergency Management Agency <br /> (FEMA) which has maps depicting FEMA-defined 100-year and 500-year flood zones. <br /> The Phase I/RFA and Closure Report indicates that the subject property is not located <br /> within the National Wetlands Inventory. This data, available in select counties across the <br /> country, was obtained from the U.S. Fish and Wildlife Service. <br /> The topography of the property is at an elevation of approximately 37 feet above mean <br /> sea level and in an area of low topographic relief. Regional slope of the area is toward <br /> the west-northwest. <br /> Statement of Basis for Former Advanced Interconnect Technologies, Inc. Facility Page 5 of 15 <br />