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i~ <br />r;. , <br />.v-- ': <br />.r - <br />~; {' .. <br /> <br /> <br />'.do :unin uou.ld occur bene,ah 2asC Sal[ Cree'-.. Icpacts <br />1:1 :!nil Jd ~.^.C ~'•1C ~vl C:!:'; I~!:1 ~;" ::rc'.1 SilnU l!! !1E` :CLnUC. r~gCC: <br />c•d :!luaCC [`:is r!C L-C r.ti ~atior. ~:+,i ::n^ neas::re•: Co nroL'ee[ <br />a buEEer zone, <br />P, q,ti, L'ol. 1. T.•rrara d,:paaiU~ is l:~~r~~-r ri+•rr vn7luy:: :err. tl•._ orincicaL <br />sou:ee o: '%rc•.:na a:~tcr. the crin2t~- _~...cr- ~~` ~ .C';.i:"r i.s irri;,alion <br />iaacrr. <br />!lrccr.c cil:r, i•~-: 110C COPS all o Che ctrC ~:~. val le;•s, mid ailere saCUraC~:•.t, . <br />i,olds th-, eater tahl•= under ur.cnnEined co~aition :\liuvial .vlui fern are . <br />in clu::e i;,draulic conr.ection.~aith a:'i~cer.C str•_ns an:! nerioaicnlly are. <br />rrchar y,r~l by or dischar¢r into the^, ~ira:•nd inC on ~:~hreher at ruace levels <br />err i:io,i? oc log:. ,':::~ poorer qu.~lit•: .~E alluvial. •.!:_Cer tcrnnan:d to s[LNaz <br />d:Ce:) is attril~,utec Co leacL•ins: o` .,^1 LS Riv .rrira[ion rc[ivir.ies and <br />y'COUr'.(1 +:r'iCt'C 1nllUt! ICOt^, u'l:l••rC;rlrl^ F..;:!rlli~. lO:'^aCli)n5. <br /> <br /> <br />:d <br />i'iC(1"( <br />III IIIIIIIIIIIIIIII <br />u <br />~ ~~~ <br />l~- <br />'Ii Lc, :;un;.rr LanVOn (C(? !%:154) nn•I ".cCl;;,.;: fanyon (CO 4i2%) <br />.7odl a :~Irrrlman <br />SUI:JECT; arferer.cee to Chc Lo: (a Prnjrct ~"ue~_r C:(nyer, and HeClane Canyon) in <br />Chr G. G_ntral Colorado Coal CIS (So^r of these references indicate <br />pot~nCially siynifican[ inpacCs) <br /> <br />A. Y.%'~' <br />i <br />i'. 93, Pol. I. !iydrologic data for surface arc1 ground eater resources <br />nrr:,'rd co identify ~7F's are not rrv~ilaSle az this time. In general,. <br />Elcux',plsins of rivers and looter reaches of r;pct pcrr.nnial and some <br />i nt.,rr..iltrnC SLCra:^.I valleys Lravr.r:: i. n:; ea s.t~rn coal areas are un:iouhted!y <br />AVI",,. !io[:C s[rea^s in 1+rsLern co;:1 ar~es_are ;;he+,e[al am+_ t+ould n:.~ <br />qua! i -, !;oCC: IC would appear free: F:i..S sr ntcn::r.ts that e~hu~eral <br />sCreara ur+• autonaticall.y ercluded from-consi,lrrn[inn as an AV?• <br />P. 925, Sul. Z. The old valley floor hordar-i:(g [he incised channel of - . <br />cast ~aL[ r: rrk is very prohnhiy an A~'F. ~ .. <br />CO .,cr C:u r. L'.lC ~: <br />Clio ... , SU~a; ilY <br />a <br />