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At !ha time of our field exploration the excevetion of the buildinp <br />ped�, eech meeaurinq epproximetely 54 Eeet eeet-wesC by 60 feet <br />norlh-socith, end placement oE the rock mate hed been compieted. <br />Pumpinq o[ en eccumuletion oE eurfece Neter wes neceesery in order <br />to complete the exploretion pite xithin the buildiny ped loceted on <br />the rorth eide of Sprinq Street. <br />Meteriels temoved from the verticel eided, buildiny ped excevetione <br />were stock-piled eround the northetn, eeatern end eouthern meryins <br />o[ the excevetiona. Sloughing from the etock-pilee hed covered the <br />verkicel cute in tSie�a ereae, end eilt had eccumuleted on top oE the <br />tock mefe. However, along the Weetern edge of the pad ereas there <br />Mes e qood exposure oE the natur�l eediment proEile to a depth oE <br />eboul�J feet. <br />7.0 BXPLOR]►TION PITS <br />The eix"exploretion pita Mere exceveted with e• rubber-Eired,• <br />tractor-mounted backhoe. Due to elouyhinp end repid water eeepege <br />within the pits, subeurfece conditione Nere interpreted beaed on the <br />digqinp ection oE 'fie beckhoe ee Nell ea eediment removed from the <br />explorelion pite. Meteriele encountered in the exploCetion pits <br />Nere etudied end cleeelEied in the Lield by e yeologist [rom our <br />[irm. All exploretion pite Nere beckfilled immedietely eEter <br />, exarnination end lopyiny. • . <br />6ubsurfece conditione et the project eite Nere inferred itom the <br />field exploratione eccompliehed for thie etudy, end vieuel <br />raconneissance oE the eite. In qenerel, the exploration pita <br />encounEered e thin (ebout 3 to 6 inchea) leyer of eilt end eend <br />ovarlying ebout 1 to 1 1/� Eee! of 1 to 6 inch querry epelle. Denee <br />to v'ery denee, moiet to Net, mottled yrey, eilty, Eine send Nith en <br />uhsorled mixture of cley, pebblee end cobbles wee encountered in ell <br />oE the exploretion pita beneeth !he querry epella. Thie meteriel is <br />interpreled to be Veshon ege (19,500 to 15,000 yeere beEore present) <br />lodpement lill. Theee eedimenta Nere ;;epoeited et the eole oE the <br />advencinq Veshon eqe ice eheet Mhicii hee reaulted in their high <br />etrangth end loN permeebility charecterietica. Due to elouphiny of <br />the Querry epells end very repid xeter eeepege in ell of•the <br />exploretion pite, the pite vrere lermineted et deptha oE J to 3 1/1 <br />ieet below the top of the rock mat elevetions. Till wae elso <br />expoeed�'ih the cute elonq the weetern edge of the ped ereas et <br />depths tenqing from ebout 1 1/7 to J Eeet beloN the pround aurfece, <br />where it wee overlain by en orpanic rich topeoil horizon, end then e <br />1syeY of surficiel fill. <br />The Neter enaountered in the exploration pits and present Mithin the <br />ped ereee ie interpreted to represent e• perched ground water <br />condition. Perched weter occura Nhen eurEece Meter infiltretee doun <br />through reletively permeable materiela end becomes trepped or <br />"perched" etop a comperdtively imperineekile barrier such ee the till. <br />It ehould be noted thet fluctuetione in the level oE the eurEece <br />Nate[ mey occur du• !o th• tim• oi th• y��r •nd v�r1�lien• in <br />r�lnt�ll. <br />'r7 <br />