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Dama, Inc. March 31, 2004 B94301.01 Page 3 2.0 SITE DESCRIPTION ` Information concerning the Site was obtained from a Site reconnaissance and a review of the documents referenced in this report. r 2.1 Location and Description of the Site i. The Site is located at 1248 W.Hammer Lane and 1301 W.Joan Avenue,in the city of Stockton,San Joaquin County, California, on one rectangular parcel. The Site is developed with a single story, wood frame residence with detached wood frame garage and barns at the 1301 W. Joan Avenue address. The 1248 W. Hammer Lane portion of the Site is vacant land. A Site location map is presented as Drawing 1, and a Site plan is presented as Drawing 2 in Appendix A. The San Joaquin County Assessor's Office(SJCAO)has assigned Assessor's Parcel Number(APN) 077-049-04 and 05 and listed the legal owner as: Herman Keesee 208 Seaside Street Santa Cruz, California 95060 ` Although the SJCAO lists the legal owner as Mr.Keesee,according to a grant deed for the property, dated December 2 2003 the legal owner of the Site is Michael G. Collins &Deborah A. Collins. 2.2 Physical and Environmental Setting of the Site r, Physical and environmental characteristics of the Site including topography, geology, soil and hydrogeology were evaluated based on Site observations,published literature, and maps. �.. Topography Topographic map coverage of the Site is provided by the United States Geological Survey(USGS), Lodi South, California, 7.5-minute quadrangle map dated 1968,photo revised 1976. The Site lies within the southwest quarter of Section 16,Township 2 North,Range 6 East,Mount Diablo Baseline and Meridian. According to the map, the Site is located at an elevation of approximately 10 feet above mean sea level, and the land surface slopes slightly toward the southwest. Areas to the northeast of the Site appear to be topographically upgradient. Geology ` The Site is located within the San Joaquin Valley.The San Joaquin Valley is part of the Great Valley Geomorphic Province,a topographic and structural basin bounded on the east by the Sierra Nevada and to the west by the Coast Range.The Sierra Nevada,a fault block dipping gently to the southwest, ` is composed of igneous and metamorphic rocks of pre-Tertiary age which comprise the basement complex beneath the valley. (USGS, 1986). The subsurface of the Site and surrounding vicinity is characterized by a thick sequence ofunconsolidated sediments. Subsurface material beneath the Site is primarily composed of alluvial fan deposits and flood plain over-bank deposits including interbedded silts, sands, clays, and gravels (USGS, 1986).