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I <br />3-8 <br />carried away in these streams. Since large quantities of soil have not <br />been observed adjacent to these seepage points, large channels within <br />the foundation may not have been generated. However, the movement of <br />wet areas or seeps from one side of the valley to the other and an <br />increase in seepage rates could indicate changing conditions within the <br />foundation. <br />F <br />