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NOV-09- <br />From; JeraldS <br />Ffield <br />Ph 1999 TUE 04:40 PM <br />D <br />H <br />droD <br />namicslnco <br />atedFat:(i(~66 <br />o FAX NG, <br />Voic <br />{3D3}841~311T <br />lt <br />L <br />riP <br />~ <br />f <br />}I <br />l <br />dlG <br />M <br />lt <br />h P, 05/10 <br />. <br />, . <br />. <br />y <br />ry <br />y <br />r e; <br />e <br />o <br />o <br />e <br />: <br />ams~a <br />o; <br />a <br />y <br />ag <br />un <br />n Pageaoryiuesary,nouemoo~ua,im~,ui.wrm <br />Ms. Lori Potter <br />Project No. 9974-01 <br />Page 3 <br />November 8, 1999 <br />close monitorlttg of this quarry, it is our opinion that severe impacts to downstream properties <br />will continue in the future by sediment yields associated with significant storm events. <br />Lastly, it is our opinion that eho Storm Water Mattagertrent Plan (SWMP) is not complete if the <br />quarry has to meet eonsauctioa site criteria. We have attached information from the Colorado <br />Department of Heahh that illustrates their requirements. It appears the SWMP does not meet <br />Colorado's (or EPA's) minimum criteria. <br />James Di111e 6/04/99 Inspection Report <br />Mr. Dillie indicates that a late April and early May storm event oectured that resulted in large <br />diameter particles being transported downstream. Such a conclusion means smaller diameter <br />particles were also transported downstream, <br />His report supports our opinion that the quarry was a significant source of sediment to <br />downsveam properties. He indicates "Stream banks worn otoded whioh increased the width of <br />the creek." Also, he states "The amount of material that was collected In the constructed basin is <br />several feet thick over I-1 acres," <br />We do not know if Mt. Dillie actually measured rho depth of material in the constructed basin, In <br />any event, his last statement deartortstrates that deposition of material must have occurred during <br />the cad of the runoff event. <br />When flows discharge tiom a sediment containment system with high velocities, little sediment is <br />actually captured by the sttucture, Only during the end of such runoff evenu will flow velocities <br />be low enough to allow foc deposition of small sized sediment particles. It is our opinion that at <br />least three to 10 times the amount of sediment collected in the construction basin actually flowed <br />downstream during t}te flood event. <br />In summary, Mr. Ditlie's report substantiates out professional opinion that stringent sediment and <br />erosion central practices must be continually implemented for this tttirting operarion, In addition, <br />enforcement of this policy must be a responsibility of the DMG. Otherwise, continual detrimental <br />impacts on downstream properties cea be anticipated whenever flood flow events occur. <br />Mr. Jo~epb M. Ricci's November 3,1999 Letter <br />We have reviewed Mr. Ricci's letter and have the following comments: <br />1. The statement about the aedimentatioa pond appears to be correct in that something <br />apparently was constructed. However, as we have stated above, the structure does not appear <br />to have been properly sized, designed, or built. <br />2. The SWMP was not properly prepared and is missing significant information. <br />3. The fine sized panicles collected at the mined area represetrts only a small portion of the tote! <br />amount of sediment that discharged i}om the quarry doting flood events. <br />4, We cannot $rrd say statement in Mr. Dillie's report that says rho back grading ".. ,assisted in <br />keeping the flow of water fiom the quarry walls in check" We doubt such s statement can be <br />hydrologically substantiated for the rainfall events that occurred on April 2g --May 2, 1999 or <br />in August 1999. <br />