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• <br /> II. SITE CONDITIONS <br /> • GEOLOGY AND GROUNDWATER <br /> The subject property is located approximately 3 miles from the Coast Range Mountains <br /> which border the San Joaquin Valley on the west. The elevation change is a very gradual <br /> • increase toward the mountains on the west The property hes at the outer reaches of the <br /> alluvial outwash from these mountains <br /> • Information gathered during the AEMC Phase II Investigation indicates that the site is <br /> underlain by silty clays, silty sands, and clayey gravels that are characteristic of outer or <br /> distal alluvial fan deposits <br /> • According to a United States Geological Survey--Water Resources Investigation, local <br /> groundwater is approximately 60 feet below ground surface (bgs) The depth to <br /> groundwater in the well at the site is 58 feet bgs (Lawrence Pereirra, personal <br /> • communication) <br /> • <br /> • <br /> • <br /> • <br /> '1h1d io(�A) Page 6 <br /> CNvbIWMiwMnlywG(w4Nl CO.# <br />