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. <br /> W. T. Duryea Company JN 87105 <br /> May 29, 1987 Page 2 <br /> Test Pit 4 was excavated in the ptoposed pazking area and <br /> found four feet of silty gravelly sand fill fzom a glacial till <br /> soacce. This was underlain by about one and one-half feet of <br /> dazk brown organic silt with roots and wood debris . At a depth <br /> of 5.5 feet a reddish brown weathered till or loam soil was <br /> observed. This pit was terminated at a depth of eight feet . <br /> Test Pit 2 also encountered about two feet of fill <br />�'�` containing large pieces of asphalt and concrete slahs . It <br />��:'_. :._ <br />,;� : appears that this'` fill was localized . The topsoil layez has <br />' been disturbed by previous clearing and giading actions , but <br /> appears to be generally 1.5 to 2 feet deep. A reddish brown , <br /> medium dense , silty gzavelly sand (weatheted glacial till) was <br /> observec� undez the topsoil . Dense glacial till was encountered <br /> at a depth of three to fouz feet below the ground surface in the <br /> proposed building area . <br />'";�� , The final logs repzesent our interpretations of the field <br /> ` logs and the results of the laboratory examination and tests of <br /> ,;,` : - ` field samples. The stratification lines on the logs represent <br /> the approximate boundary between soil types . In actuality, the <br /> �,�-- transition is more gradual . <br /> ��.i_-,-�: <br /> �il°r��:; GROUNDWATER <br /> Gzoundwatez seepage was observed at a depth of 5� 5 feet <br /> in Test Pit 1. No seepage was observed in the other test pits . <br /> It sho��ld be noted that groundwater levels vary with rainfall <br /> and rther factors . We anticipate that groundwater could be <br /> found between the neaz surface weathered soil and the underlying <br /> glacial till and in more permeable soil layers or pockets within <br /> the till soils (fracture zones in silts and clays) . <br /> aYs'3` ,.. . <br /> 6Y <br /> CONCLUSIONS AND RECOMMENDATIONS <br /> GENERAL <br /> The native soils below the topsoil and fill soils will <br /> provide excellent support for the proposed structure. Site <br /> preparation work will begin by clearing all existing trees . <br /> Then the urganic topsoil and fil; soils should be removed fzom <br /> the building area. A stripping depth of one to 1. 5 feet in <br /> areas not having fill is anticipated. At the location of Test <br /> Pit 2, about 3. 5 feet of soil should be xemoved . We understand <br /> GEOTECH CO\SUI.IAV'fS iNC. <br />