Laserfiche WebLink
T f <br /> 19 March 1999 <br /> AGE-NC Project No. 98-0471 <br /> Page 2 of 12 <br /> sedimentary formations range in age with the older deposits being primarily marine in origin and the <br /> younger deposits being primarily continental. Continental-derived sediments were primarily <br /> deposited in lacustrine, fluvial, and alluvial environments with sources being the mountain ranges <br /> surrounding the valley (Olmsted and Davis, 1961). The site is located on unconsolidated and semi- <br /> consolidated alluvium, lake, playa and terrace deposits of Quaternary age (California Division of <br /> Mines and Geology, 1977). <br /> The Modesto, Riverbank and Turlock Lake Formations and overlying Recent alluvium are the <br /> principal sources of domestic ground water in the 13,500-square mile San Joaquin Valley Ground <br /> Water Basin (Basin 5-22). Ground water occurs in a generally sandy clay layer extending from <br /> approximately 6 feet bsg to an unknown depth. <br /> 2.2. GROUND WATER DEPTH AND FLOW DIRECTION <br /> Based on the San Joaquin County Flood Control District and Water Conservation District Lines of <br /> Equal Depth of Water Wells Fall 1996 map no relative information to estimated depth to ground <br /> water is available for the site area in western most Stockton, except that ground water elevation <br /> contours are less than 10 feet below surface grade(bsg). Based upon information obtained from the <br /> AST assessment, ground water is currently at a depth of approximately 5 feet below surface grade <br /> (bsg). Ground water flow direction is unknown and may be highly variable. <br /> 2.3. REGIONAL HYDROLOGIC SETTING <br /> The Middle River is the nearest surface water feature to the property, located approximately 500 feet <br /> south of the site. Water from the channel drains into the San Joaquin River and is primarily used for <br /> commercial and recreational boating, with agricultural as a secondary use. The channel contains <br /> water continually and potentially has a tidal effect upon ground water depth or flow direction in the <br /> area. <br /> 2.4. ON-SITE RECONNAISSANCE <br /> In June 1998, AGE personnel visited the site at the request of Herum, Crabtree et al, to identify <br /> locations on the property that potentially have subsurface impacts resulting from past and current <br /> site usage and related environmental concern area. Three area,of concern were noted: a large (7,500- <br /> gallon)diesel AST which appeared to be leaking fuel from the dispensing location onto the dispenser <br /> pad;a smaller operating (approximately 1,000-gallon)AST with a portion of its system lines buried; <br /> and an area used for waste oil handling and possibly disposal. <br /> Advanced GeoEnvironmental,Inc. <br />