Laserfiche WebLink
2-3 <br /> Sierra Nevada Mountain Range, and east from the Costal Ranges, towards the center of the <br /> ' valley, then north towards the Central Valley Delta area The general groundwater flow <br /> direction in the Stockton area is reportedly to the northwest, towards the Stockton Divertion <br /> Channel, and exists at approximately 75 to 100 feet bgs Shallow groundwater is considered <br /> ' unconfined and has been designated as a beneficial water use unit Groundwater is used for <br /> farming and ranching (tmgation of crops and watering of farm animals), municipal and <br /> industrial water supply, and as a drinking water supply for the general public <br />' Local Geology Y g gl'and H dra Bolo . The Site lies at an elevation of approximately <br /> 25 feet above mean seal level Sediment deposition in the area has produced nearly horizontal <br /> topographic features in the vicinity of the Site. Soils encountered beneath the Site, during <br /> previous investigation, consist of interbedded alluvial deposits, including clays, silts, sands, <br /> and fine gravels <br /> The San Joaquin River is located approximately 4 miles southwest of the Site <br /> However, the nearest body of surface water, a water transportation and irrigation canal, is <br /> approximate one-half mile northeast of the Site Groundwater has been encountered beneath <br /> the Site at depths of approximately 75 to 85 feet bgs Groundwater has been identified as <br />' flowing from the west-southwest to the south-southeast, beneath the Site, at gradients ranging <br /> from 0.0004 to 0.0013 feet per foot The reason for the apparent discrepancy between the <br /> local and regional groundwater flow direction is unknown <br /> Use or disclosure of data contained on this sheet is subject to the restriction specified at the beginning of this <br /> document <br /> OS118195W-NREPOR751156T100966kCHAR2 W P5 <br /> QMS-PS410 <br />