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The Leadville Mill M 1990-057 <br /> EXHIBIT C—MILL PLAN <br /> Page 4-32 <br /> eFessing undeF two aeceSS Foads. The channel flows Onto what appeaFS to be an e[d <br /> then flews along the EeRtOUF tO the neFthwest, exiting the pFepeFty on the westeFn <br /> peanaar . YRdistwbed aFear-aneffwater—ze the neFth of the unnamed dFainage <br /> One type of sea! elassificatien exists within the the Fead aFe 12in EulveFtS, With ne evidence ef eveFtepping OF wash outs. The wateF <br /> the Lake County SEA SuFvey. The semi seFffies is Leadville sandy lown (LeE). This is a <br /> vv v v a i an a sviT—riTePi ca em�p ate-tf ee en the p f ep cfzy-1s L9 crgepvre- H Pone. <br /> te—geneFally fellew the same paths as the hiSteF;E basin SE aetenistics are <br /> Wentaeal to these ef the histoFic basin, except fo i I building, impeundment <br /> area of the PFE)jeet. Swales and Inlets aFe designed to handle the 100 year 24 heur <br /> peak flew. <br /> fence,a Fe S i e n Eo ntFel 4egs,EeRStFW EtiE)n eTtFaneesreek (OF OR site ee huh I e� <br /> er gFaveled and maintained as seen as ffactical. <br /> ( 1) nlatUFe of Milling Aetivi+ies at the Site <br />