Laserfiche WebLink
Former Discovery Chevrolet June 5, 1998 <br /> Tracy,California Corrective Action Plan <br /> diversions and redistribution of surface water throughout the area. Groundwater quality in <br /> the water-bearing units of the San Joaquin River Basin is generally fair to good (meets <br /> recommended secondary or primary standards for drinking water). <br /> 3.3 Local Geology <br /> The site is located in the northern portion of the San Joaquin Valley in western San Joaquin <br /> County, California. Unconsolidated continental and lacustrine deposits of Holocene and <br /> Pleistocene age underlie the northern portion of the San Joaquin Valley. These deposits <br /> consist predominantly of unconsolidated fine-grained materials, with buried channels of <br /> sand and gravel. These deposits are underlain at depth by coarser-grained water-bearing <br /> continental sediments. Reported subsurface materials encountered during drilling at the site <br /> consisted primarily of fine-grained soils such as silty to sandy clay, clayey silt, and clayey <br /> sand. Intersecting cross-sections through the area of investigation were included as Figures <br /> 4 and 5 in Horizon's Problem Assessment Report. <br /> 3.4 Local Hydrogeology <br /> The most productive water wells in the Tracy area are those wells completed within the <br /> Lower Aquifer Zone of the valley alluvium. The valley alluvium consists of permeable <br /> continental and lacustrine deposits interlaced by numerous gravelly stream. According to <br /> DWR records, the nearest well to the site is 700 feet north-northwest of the site and is <br /> completed to 427 feet bsg. An apparent water well discovered outside of the northwest <br /> corner of the service bay area at the site was measured to a depth of approximately 145 feet. <br /> The shallow groundwater being monitored beneath the site is within the uppermost water- <br /> bearing or water table zone. Shallow groundwater generally occurs in the uppermost water- <br /> bearing zones in either unconfined or semiconfined conditions. Because of the generally <br /> fine-grained nature of the shallow water-bearing materials and poor historical land-use <br /> practices, shallow groundwater in the area is no longer utilized for domestic purposes, but <br /> ' .; may still be used for agricultural irrigation purposes. The shallow groundwater beneath the <br /> 3001-21.cap 6 HORIZON ENVIRONMENTAL INC. <br />