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143-260-08-1; it' s location is shown on a portion of the County <br /> Assessor' s parcel map -- A&ENDIX A. <br /> REGIONAL GEOGRAPH C SETTING <br /> The property is located just east of Highway 99, between Waterloo <br /> Road, (Highway 88, ) and Fremont Street, (Highway 26 , ) about 2-3 <br /> miles east of City Hall. The area is zoned for manufacturing and <br /> light industrial use, there are no residences in the immediate <br /> area. The Stockton Diverting Canal is a short distance to the <br /> east, and a spur of the Stockton Terminal Eastern RR is dust to <br /> the south. PLATE I gives more details of the immediate area. <br /> GEOLOGIC & GEOMORPHIQ-PROVINCE <br /> The site is located near the southern end of the Sacramento <br /> Valley about 1 1/2 miles south of the Calaveras River and 3 miles <br /> northeast of the Stockton Deepwater Channel Sediments in this <br /> area have been derived primarily from reworked material from <br /> • meandering streams and flood plain deposits. The original source <br /> is outwash and erosion of the volcanic and metamorphic rocks <br /> formed during the uplifting of the Sierra Nevada Batholith to the <br /> east. The topography is one of very low relief , with drainiage <br /> towards the west-southwest at about 5 feet per mile. PLATE II is <br /> a portion of a USGS quadrangle sheet showing the location of the <br /> property is relation to surrounding geologic features <br /> SOIL TYPES <br /> According to the 1952 publication issued by the University of <br /> California, Berkeley, surface soils in this area are classified <br /> as Stockon Adobe clay, which is derived from reworked basin <br /> sediments. It is generally dark gray, fine textured, with a <br /> Storie Index of 24. It is typically underlain by calcareous <br /> subsoils containing hardpan or hardpan-like substratum. The <br /> sediments encountered at this location generally conformed to <br /> that description, except at the southern end of the excavation, <br /> where a lense or pod of sandy clay was encountered PLATE III, <br /> showing general soil types in the area, is from that 1952 <br /> publication Detailed description of the sediments penetrated by <br /> the soil borings and monitoring wells are given later in this <br /> report. <br /> DEPTH TO GROUNDWATER <br /> A review of San Joaquin Co. Flood Control Maps indicates that <br /> 2 <br />