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PERMFILE43198
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PERMFILE43198
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Entry Properties
Last modified
8/24/2016 10:45:35 PM
Creation date
11/20/2007 11:28:53 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1988044
IBM Index Class Name
Permit File
Doc Date
7/22/1988
Doc Name
COAL CREEK RESOURCES FN M-88-044
From
TUTTLE APPLEGATE RINDAHL INC
To
MLRD
Section_Exhibit Name
EXHIBIT C D
Media Type
D
Archive
No
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~= <br />~..~ <br />TUTTLE APPLEGATE RINDAHL, INC. <br />'~ Consultants for Land and Resource Development <br />Mr^. Sohn Dner^Per• <br />Mired Land Reclamation Divisio+•~+ <br />Scaly GG, 1988 <br />Page 4 <br />The lowering of the gr•~+_~ndwater table will have a min~~r• <br />impact on the pr•i~+andwat er table upstream of the n7l ni no site. <br />Once nrater•ial has been removed, the aquifer will attempt to <br />reach a state of eb~.iiiibr•ium. This will mean that theta <br />gr•o+.+ndwater^ table in the immediate vicinity of the mine will <br />Iower• and discfiar•ge ^r•o+Indwat er at a ^r•eat er• volume tfian il: <br />pr•ev iously has f.~r• a short period of time. however, this <br />drawdown effect will not extend up the fail Length of then <br />valley. Since the mining ~~aer•at it~n will take tw~~ t~~ three <br />years for- tfie full impact of removing the sand to be felt i+•i <br />any ~~ne area, this lower-ing 1s n.~t s~~nreth ing that is going <br />to happen overnight. <br />Mast mining oper•at i~~ns along the S~~+atfi Platte River- that- use <br />wet mining techniques gener•aI Iy Lower- the +apper side of the; <br />water table by S to B feet. T`n is creates a drawdown on the <br />+xpstr•eam side that generally runs ~~+at within ?,O+D feet ~~f thea <br />mining area. The Snrpacts of this project wiil be greater <br />because ~~f the iar•ger• drop in the water table. It i~~t~ <br />expected that the water- table will reach eq+ailibr•1+_~m within <br />1@+D+D feet of the minin^ site at Coai Creek. Rougf+ <br />caiculat ions using She equ1116r i+_im equation for drawdown in <br />an uncinf fined aeuifer• sfiow that the read i+as of infl+aence irr <br />appr~~xintately equal t+~ the radius c+f the mining area if <br />projected into an equivalent cir•c fie. <br />Hggradation at tfie l~~wer• end .,f the mining site again is not <br />a significant Pactor• in this mining plan. We are dealinc) <br />witfi ari ephemeral stream that does not m~~ve mucfi material. <br />Eedload is very iow since the flows ar•e generally not great; <br />enough t+~ over•c~~me tr^active forces. Suspended load canrn~t <br />be Large because +~f the simble Lack of total voi+ime of flooa <br />avai labia to carry a s+_isoended l~~ad. The ~~niy time y.,u wi i I <br />see a significant movement of material in tfiis area is:> <br />d+a r^ing low frequency storm events. In this instance, it <br />d~~es not matter- whether- there is a mining oper•at ion in thra <br />area or• not, material is g~~ing to be moved. Eased on the <br />flows we have calculated, aggravation is not g~~ing to be ai <br />problem with this pr~~,7ect. <br />Channel degradat iun at tfie cost ream end .~f the gr•o,]ect will <br />be handled 6y constr+~ctinp a cfiannel drop and r•+and+~wn irate:? <br />the mining area. This str•uct+are will be designed acc~~r•ding <br />to Ur^ban Drainage st andar•ds. In thla manner^, we will. <br />pr^eciude er•os i+~n and headcutt ing +_~ostr•eam •7f the mining <br />site. <br />
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