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i <br /> KLEINFELDER <br /> The depth to the static ground water was measured on March 23, 1989, from a set location <br /> at the top of each PVC casing (TOC). The depth to water was subtracted from the <br /> elevation of the top of the well casing to provide'.'a ground water table elevation for each <br /> monitoring well location. The well elevations, depth-to-water measurements, and <br /> calculated ground water elevations are presented in Table 2. <br /> The ground water elevations for each monitoring well location indicate an apparent ground <br /> water flow direction to the northwest. The gr`'ound water table elevations, estimated <br /> ground water elevation contours, and estimated ground water flow direction are shown on <br /> Plate 3 (Estimated Ground Water Flow Direction" <br /> Y <br /> i, <br /> E <br /> r <br /> 175-89-543 7 <br /> k <br />