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-- wrtiicc lnycr is reddish hrotcn line sanely loam about ?; inches Ihlck. l he <br />-• unJerlying material In reddish hn,t,'n :utJ light reddish brat+'n k,;un about _'!+ <br />Inches thick atcr velluwish red strutiticcl loam and sandy h,ant. Pernuability is <br />_ nnaicratc:unl the at'ailuhlc tsatcr capacrtc is high <br />-- 1'hc fiarrtum series cnnslsts of derp. well drunnl soils thin li,nnc,f in allu\ ium <br />-- ham reddish culanJ shale and sundsh,nc l he surtacc I:R'er Is it pically hr\+tt•n <br />--_ Inam ahl+ut 10 Inches tltiek The underh utg m;ueriul is reJCilsh hn+ttn lam <br />ar.llltieil with thin lu~'cr~ ul sanJ~ Il,;un and i about lit inrhe. tlu~k. <br />_ Penmahilin• I> moderate anJ the at citable t~'ati:r c:Ipaclh is high. <br />-- 1 iir Cunncnnn-liamurn a+mplcL rcpunccily occurs alum the tiurih Pnudre tiupph Canal <br />- ^nJ adjuccttt to the tvestcrn hnundan ut the proposed prrmn area. It also repunell)' <br />_ _ occurs along I 'ti Hielucay _'+;'. earl of the mine site. <br />-- Pumer tine .anctr taunt. 1 to U0o slopes -This nearly lovel to su~ongly slupiug sail is nn <br />-- thr uplands and ridge>. it consists of shallot+. tce•ll drmned soils that limned in materi:J <br />-- tvcathercJ th,m reJJislt hri,tt'u sandstone. 'I'hcsc soils arc on uplands and an underlain <br />__ by smtJsa,ne at a depth of 1f1 to'n inches. 'Cypically, the surface layer' is reddish brat+•n <br />-- (isle sands' loam ahuut ?inches thick 'fhc underlying m.ucrl:tl Is fight n•ddish hrmcn line <br />-- sanclt loam about '' Inchcc thick. Bclut+ this Is hard redJtsh hn+tvn sandstone. <br />-- 1'ermcahihtt is moderate and the ataiiahle tt•ater copacit} Is Ima- These soils rcpunedlr <br />-- ~ cur southwest of the pn+p cscd pcnnit area. <br />-- • I't:mei-hock i,utcrnp a+n,plCX. I it x+ X1,1" i, slopes - This catnplc~ rnnsists o1' moderately <br />-- ~Iccp or steep oils un upl;uxls and ridges. It is about i$"„ Pumer tine candy loam and <br />-- chow 3(1"„ ruck ouun+p. Pumer line sandy loam is snuniihcr mid less slopin_~. .4 small <br />_ _ arc;a of this soil rcpc,ricd occurs hetn•ectt the sou;hem end of the proposed pcrnut area and <br />-- l!S High\t'ay'_87. .A typical profile oi'this Pumer soil is dcscrihed m thc• praeding <br />-- paragraph. <br />-- l:Irtlry Pumer aunple~. ~ to'_il"~~ sli,pes -This complc~ consists of strongly slopinc to <br />_ _ moderateh steep sell. nn upland and ~-alley sieics. his about 4~"„ Kirtley loam and <br />-- ;flout dtN4~ Pumer fine sandy loam. Rtnlet loam is snuu,thcr and Icss slopine.:utd the <br />-- Turner a steeper. <br />-- l he Purnrr soil is dcscrihed in the prccuiima parueraphs. <br />-- The I~inler• Inane consists of moderately stoup, well drained soils that formed in <br />-- material weathered from reddish hrotvn sandstone anJ shale. Thcsc sails arc nn <br />_ uplands wtJ side slopes anJ arc tmdorluin M sots shnle ut a depth nf'~ to -41) <br />_ iact•~c~. iyptcaly. the suraace layer is rcddi.h brut~n loam ahuut -1 utchcs thick. <br />l he subsoil is reJJlsh brown heat} loam about I ~l indics thick. Pcrntuahility is <br />- moderate rind the atailahle t+•ater enpacitc is mudtum. This soil cample~ <br />- R'Ir. ~t'1 C'~II\ ~J::i llr> ltlii;li'L'71f il~ lhi :V ,'rtl l\C>i h("'t li Kl (,l Illy t,l'~~p,~se\l i,~:,lllt ^rd:1 <br />__ • <br />1 V <br />