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, .: __. .--... <br /> 1 <br /> ( Powder Milt Creelc. Howevcr, as desccibed in the �xt secrion, m�st of ihe ground water <br /> recharge w the crak is finm a daper n,ional �quifer. <br /> i" <br /> A.. Q,�R�io�l �tar�h A +�q '� �r Imn� <br /> , The ground waur within the rcgional outwash aqui:`er provides most of the rechazge W sapages <br /> 1 an:, springs in the upper portioas of the drainage ravias, and coutn'bntes w most of the snrface <br /> flow in these drainages. The recharge to this ground water regime is iaterpreted to be primarily <br /> ( ;`rom regional off-site sources. In addition, the regional outwaah sedi�nts are capped by very <br /> low permeability lodgemem ti11 or silt units, which reduce recharge from overlying on-site <br /> sources. Therefore, consaucdon at the site should 6ave li�'s impact to grou� water in the <br /> ( ngional outwash aquifer. <br /> � <br /> � <br /> � <br /> I <br /> � <br /> J <br /> I <br /> 1 <br /> J <br /> I <br /> ] <br /> l <br /> I����� <br /> �� <br />