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Page 4 - #120-11872 <br />Fine, coarse and mixed alluvial deposits were encountered at several of the <br />boring locations. Generally these soils were encountered immediately below <br />the topsoil. The fine alluvial deposits consist of silty clay and clayey <br />silt. These soils have soft to medium consistencies. In a few of the boring <br />locations, some granular coarse alluvial deposits were also encountered. <br />In the eastern lower portion of the site, these soils are loose, however, <br />in the higher portion of the site at boring 6, these deposits are dense. <br />The glacial till deposits consist primarily of sandy clays with some lean <br />clays and clayey sands. Generally, these soils have a soft to medium consis- <br />tency in the upper portion of the deposit and become rather stiff to very <br />stiff with depth. The softer glacial till deposits were generally encoun- <br />tered in the lower, eastern portion of the site. <br />Water Levels <br />Water level measurements were made in the borings and the data is included <br />on the logs. Water levels recorded in relatively impervious soils may not <br />be a reliable indication of the static ground water level, even after several <br />days of observation. The ground water levels, can be expected to flucturte <br />both seasonally and yearly. <br />SOIL t?XPLORBtlon <br />v <br />