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and are interpreted to be the primary water-bearing units within the saturated zone. Sand lenses <br /> are notably absent or rare in the east-central portion of the site, to a depth of approximately 110 <br /> feet bgs. <br /> Groundwater at the site appears to be generally under confined conditions and the potentiometric <br /> surface has been as high as 23 feet bgs (Metcalf& Eddy, 2000b). Groundwater appears to flow <br /> generally towards the north-northeast in both zones, although the flow in both zones has been <br /> variable. The various water-bearing zones do not appear to be in direct connection with each <br /> other within the boundaries of, or in the immediate vicinity of the site. <br /> 5 <br />