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1 <br /> phenomenon is frequently encountered in excavations This <br /> "perched" ground water was then encountered during the installation <br /> of the two monitoring well borings mentioned above (MW-5 and MW- <br /> 2A <br /> Potentiometric surface maps prepared individually for Sites #1 and #2 <br /> have consistently shown ground water flow directions to be toward the <br /> south-southwest The predominant flow direction appears to be away <br />' from the Stockton Deep Water Channel, which lies immediately north <br /> of the property line Tidally induced water level fluctuations in the <br /> channel appear to be the cause of slight-to-moderate variations in the <br /> ground water flow gradient <br /> Ground water wells are a common source of potable water in the Great <br />' Valley geomorphic province However, no water supply wells are <br /> located within a 2,000-foot radius of the West Weber sites <br /> 2-3 <br />