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�:-; �:, <br />graY or reddish brown, with a slightly higher silt content. <br />'The weathered zone al�o cantained some fine roots. Glacial <br />TILZ was generally disclosed under a thin mantle of FILL <br />or SOD within the Southern and Western areas of the project <br />site at depths of about 1.0 to 2.0 feet below the gro�d <br />surface to the bottom of the test pits, GLACIAL TILL <br />was not disclosed below the FILL in;test pit TP-7, GLACIAL <br />TILL soils were also disclosed beneath t he SILTS in the <br />northexn, lower elevation project areas (except test pit <br />TP-11). <br />Groundwater was encountered in all test pits (except TP-10). <br />The nature of the groundwater observed was slight to moderate <br />seepage of water above very dense GLACIAL TILL or very stiff ` <br />SILTS. However, a significac�t iuflux of water was observed in <br />Test Pit TP-7 below the FILL soils. These conditions, in our <br />opinion, represent "perched" water conditions in which surface <br />water infiltrates the upper soils and is "trapped" above the <br />relatively impermeable SILTS and GLACIAL TILL soils, Seasonal <br />variations in precipation would cause changes in the recharge <br />and consequently the quantity oE groundwater on the site. <br />GEOTECHNICAI, ENGINEERING STUDI�S; CONCLUSIONS AND RECOI�NDATIONS <br />Consideration of the subsurfac� conditions and the anticipated <br />building locations, formed the basis for the engineering 3turiies, <br />These studies were directed towards site preparation, structural <br />fill, use of on site soils, allowable bearing pressures for <br />shallow foundations, estimated settlements, slabs-on-grade, <br />parking and paved ;ireas, and excavations, backfill, and drain- <br />age requirements, Our conclusions, based on these �tudies, are <br />given in the foll.owing sections. <br />The reco�euaations submitted in this report are based in part <br />upon the data obtained from the 14 test pit explorations, �e <br />