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<br />Tc6L•h1C.2J.. n:.2.L't~io <br />AkCU Unal :~:inine Uoayany, a division of 2,tlsr.tic nichLiP1U Goal Gocpany, <br />lla6 su'ur7itteu n ~inP plan dPncriuin;; yrnpnsPu coal sirtinb and reclfiea[inn <br />OyPraC 30Ra Ln7 CnP exC ZacC LOR OL coal. ton prOyO6rd r.[. Gunnison x1r.P 16 <br />in Gunnison t.nunry in i.. 5u 1., 'Ips. 13 nr.u 14 s., 6tn Principal rrriuiai: <br />east of SbcersPt, Colorado. tlr. crops[ :1, i:ucnts is kianag,Pr, ka. Gunnison <br />rrnjPCt; jjj ~PVenteentil D[rert, i'.U, hox SsUU, lienver, Cnlnra~n, bG217; <br />phone (3U:)57j-7u14. <br />Tor pro~PCt is al undrrgrnun~ wine nn the k' seem, tnP uppersost ni sevrrsl <br />seats, aoovP tnP bear .:inP vaich is on the (: sPaW. Initial prnaur.rion i, <br />plannr•a for 300,000 tnr.a per yrar, increasing [0 1.4 eillinn [or.s prr yesr <br />uy 1`Jto, deper.dinG on sales contracts. Ul[iuately, production say reacu <br />2.S cillion tons per year. <br />GiOLGui <br />TbPrP are sis najor coal sea.~s located on the prnprrty. iuey are desi~- <br />nated A-k, vitn A heir.;; Ltlr. LOtie9C. The interval uetvepn aP.aGS varies <br />f rn.~ ]~ to 2jU tent. ltle fiCfiLS ere in tnP upper Cretaceous tiesavcraP <br />Urnup vnich is over tnr nancns S:laie. <br />~~ ihP genersl o nloGy of this per[ion of tnP snutnrast yieeance basin cor.- <br />siatfi of gently i~-:. c: dipping bed6 et 6bRaACnRP6, shales, and coal. Tar <br />prnprrty is lncateu in eountainoua terrain disaecred by rtunPrnus drain- <br />eE~s, valley walls are :SndPrBtP.ly 6tPPy anu ~er.Prslly V-snayed. Eleva- <br />[inns ntl [t:e property ranee frn~ j,90U tPPr in [he vicinity of >ioWPrset in <br />tnP valley of t:nP linrtil Yoe:: of [hr Gunr,sinn LLiv~r to about 9,]UU feet in <br />[t1P sout:tvrst corner of the prnprrty. hest of tt1P loser property is <br />oetveen 7,000 sod 2,000 tt elevation. GvrrburaPn above [hP r' sear rsnrPs <br />irn^ nil (it ourerops) to over 1,000 Pert. Un sverarP i[ vi 1'1 bP ir. ute <br />ran=r of b0U-7UU [Pei. <br />[.n Known taultinG exists nn tor- property. <br />t.unrrnus, previous, slope LailurPS and rockfalls nave seen id.ntiiiec. <br />t.ost of tuP sluaos are oPlirvPd cn be 2orr closely relates [n rot atinnai <br />siicrs tnan to arCria !lows. <br />'L.tP portsl6 nt tnr ~-9Pu.1 tine will u._ in an errs o: covereu slope ar._ <br />p Pt:a-G Otl60llaat Pa siucy uacric. <br />i.:,Gv icentitiru ana capyPU llve ;:rolo~.ic [actors capaolP of influencir.~ <br />sinln; (1 j sanusconP cnannel uP ens l[s ir, tut• root rnr. ~.; (~) proainent <br />tr.:cturr znn~s; (3) nyarnln~y; L:.) voaulPnr.;,, aua (S) steep copn~rar,i. . <br />.:PCnt:nitinn of [nrsP ![ernes anu eaPC;ustr pl annin;; will sini=ize tr.,cacr~. <br />ou cn~l Pztrutln:.. <br />~a <br />.7 <br />'i ~I~ i,~l l~~~~ ~~ il~ ~II ~~ <br />