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2 4,000 gallon gasoline tanks <br /> 1 3,000 gallon gasoline tank <br /> 1 8,000 gallon gasoline tank <br /> The UST's were removed by RAMCON on February 5, 1988 and transported to <br /> A series of site assessment investigations occurred between 1988 and 1997 <br /> The Yearings apparently sold the property at some time in the late 1990's and the property <br /> changed title at least three times In 2001 Mr Jose Garcia purchased the property and <br /> became the Primary Responsible Party <br /> On February 5, 2003, Mr Garcia retained this office to represent him and prepare and <br /> submit an expanded site investigation work plan to PHSEHD <br /> The Primary Responsible Party is Mr Jose Garcia, 521 North Cherokee Lane, Lodi, <br /> California 95240 (209) 333-0182 or (209) 365-7262 <br /> Consultant contact is Mr Stephen G Muir, Consulting Geologist &Geophysicist, PO <br /> Box 152, Woodbridge, California 95258-0152, (209) 369-9421 or (209) 601-6694 FAX <br /> (209) 369-9358 e-mail sgmuir@earthlink net <br /> The Lead Regulatory Agency contact is Mr Harlan Knoll, San Joaquin County Public <br /> Health Services Environmental Health Department, 304 East Weber Avenue, Third Floor, <br /> Stockton, California 95202-2708, (209) 468-3442 FAX (209) 468-3433, e-mail <br /> hknoll@sjcehd com <br /> The California Regional Water Quality Control Board-Central Valley Region (Region <br /> 5) contact is Mr James Barton, 3443 Routier Road, Suite A, Sacramento, California, <br /> 95827-3003, (916) 255-3000 <br /> 3. SITE MAPS: Site maps are included as Figures 1 to 4 <br /> 4. TOPOGRAPHY, GEOLOGY, AND HYDROGEOLOGY: The site is located in a <br /> relatively flat area of the southern portion of the Sacramento Valley at an elevation of <br /> approximately 52 feet above msl (Figure 4) The site is located in the central portion of -� <br /> the Great Valley geomorphic province, a north-south-trending valley approximately 400 <br /> miles long by 50 miles wide, the northern portion of which is referred to as the <br /> Sacramento Valley The surface of the Sacramento Valley is composed primarily of <br /> unconsolidated, Pleistocene (1 6 million to 11,000 years ago) and Recent (11,000 years <br /> ago to the present) alluvial sediments <br /> Mai nDEnvironmental\ParmarTexaco\Workplan\042003 wpd 4 <br />