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�DRAFT <br /> GROUND WATER CONDITIONS <br /> We did not observe ground watu seepage tn any of the test pits excavated across the site. <br /> Sand pockets encountered in TP-6 wae wet, 6owever, and we observed free water on the surface <br /> of gravel clatts wit6in the glacial till in most of the test pits. <br /> T1�e only ground water seepage encoontered in any of the borings was at a depth of 32 feet <br /> in B-1. We installed a piezometer in this boring to monitor the ground water over time; <br /> meazurements taken oo June 3 and 4 indicate a stadc ground water surtace at a depth of 29.7 feet <br /> (conesponding to an elevation of 518.3 feei). <br /> CONCLUSIONS AND RECOMMENDATIONS <br /> GENERAL <br /> We wnclude that geotechnical site conditions aze favorable for the proposed North Parl•ing <br /> Lot and for the development of future buildings at the site. Based on our site reconnaissance and <br /> subsurface ezploratior�s, tt is our opinton that tumre buiid[ngs developed on the aite may be <br /> supported on shallow arread footings founded on the native dense glacial till soil. R'e <br /> recommend reconditfontag tl�e weathered glacial till soils if foundation elements will be supported <br /> in this stratum. <br /> The surficial weat�ered portion of the native glacial soiis includes significant organic <br /> material which should be stripped and reserved for landscaping areas or removed from t6e site. <br /> 7'he lower portion of the weathered mne may be used as structural fill provided the soil is <br /> reconditioned and the organic material is screened and removed from the site. Beneath the <br /> weathered portion, the native glacial soils will provide an excellent source of savctural fill <br /> provided the moisture conteat does not substaatially increase. <br /> Glacial till consists of a heterogeaous mixture of gravel, sand, aod silt which frequendy <br /> includes cobbles and boulders. Because of the silt content, the soil is moisture-sensitive and can <br /> become easily disturbed and virtually impossible to compact when wet. For this reason, we <br /> recommend that construccion be completed in the drier summer o- carly fall months. We are <br /> presenting detailed recommendations for each geotechnical clement of the proposed development <br /> in the following sections. <br /> SITE PREPARATION AND EARTHWORK <br /> General <br /> 'Ibe subsudace soils consist of moisture-sensitive silty sand that can become eaai�y disturbed <br /> w6en wet. Uae of these materials ac stnictural fill will not be possible and vafficabiliry will be <br /> difficult during wet weather. If wet weather construaion is necessary, all excavated wee loose <br /> soils will need to be removed from ihe pavement area and replaced with "select grae�ulu" <br /> borrow. If earthwork can be completed during the drier season, the glacial soils are suitable for <br /> use as structural fill. Based on the moisturo content of tbe samples obtained, we ezpect that <br /> moisture conditioning(aerating)will be necessary for the upper soils in the weathered glacial till. <br /> 6 e o E n � I o e e r � 4 FIe No.0120-134R10/062:92 <br />