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GANSIOM IA TJAN ht ASSO(J.iTVN* <br />Hydrogeological and Environmental Consultants <br />flood his property. These flows would correspond to peak flows of approximately 10,000 <br />cfs at the Fort Lupton station if the station existed at the time. <br />35,000 <br />I <br />30,000 <br />25,000 !} <br />C 20,000 - <br />fi <br />15,000 <br />10,000 -- - -- <br />u <br />v 5,000 <br />t <br />0 <br />c°h <br />rn <br />Figure 3 <br />Peak Flows at Henderson <br />South Platte River <br />The L.G. Everist pit was lined in April 2004, and as of August 2004, the Bachofer property <br />started flooding and has continued to flood with flows of 6,440 cfs at the Fort Lupton gauge. <br />Figure 4 <br />Slurry wall constructed <br />E <br />around pits <br />t <br />1 <br />" <br />Prior to slurry wall Property floods <br />no flooding occurs '" with flows over <br />Henderson <br />7,000 <br />with flows over 7,000 cts post <br />Flow <br />-- <br />1,000 cfs. slurry wall <br />6,000 <br />- - -- <br />°,—°°-Slurry Walt <br />y = 0 9042x - 70.194 <br />Fort Lupton vs <br />0 5,000 <br />R' ° 07367 <br />Henderson <br />M 4,000 <br />o <br />0 <br />Date <br />O <br />N <br />N <br />N <br />Q) <br />tD f( <br />O <br />The L.G. Everist pit was lined in April 2004, and as of August 2004, the Bachofer property <br />started flooding and has continued to flood with flows of 6,440 cfs at the Fort Lupton gauge. <br />Figure 4 <br />5 <br />Fort Lupton versus Henderson <br />E <br />Peak Flows 2003 -2012 <br />9,000 <br />8,000 <br />7,000 <br />-- <br />6,000 <br />- - -- <br />y = 0 9042x - 70.194 <br />Fort Lupton vs <br />0 5,000 <br />R' ° 07367 <br />Henderson <br />M 4,000 <br />Linear (Fort <br />o <br />p3,000 <br />__ __ __ _ ____ ___ . _ <br />Lupton vs <br />Henderson) <br />2,000 <br />1,000 <br />0 <br />0 <br />2,000 4,000 6,000 8,000 10,000 <br />Discharge (cfs) <br />5 <br />