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were
<br />he la
<br />~~ ~ place anurface yer varies ennxs CoQV2Y COLORADO
<br />within din places is calcare reaction fro
<br />• ffcr
<br />tlon Soma areasrtaresl~Seces and ranges~f omp2stdt O ptvldely Baca-Ibrown8 7nrhes Pale-brown
<br />steep,gipa~shallow d fo~ ran tfl~lbut the ° 8 Percent. snban [IOYR o/3) when t10YR gy3we kn
<br />7pn_ g00 + Or t 50173 are t00 thin Kolar bipcky strac u~QS[; ver
<br />Much pf C anagement, for cultivation Patchy clay fll ~ hard,
<br />:uit' Iris land or twins lime i ms °a Weds; Irtab,
<br />sand and gravel type is rn idl Clca- gradual, smoeya7nt sptotehes~ modern tCOeiy a
<br />ing, Such areas' and thereafter A Y being mined for IS to 23 inch boundary. '
<br />back are used as not usab]e for far roam, eS' ~etY Pate brown
<br />filled wlth ~ dtii77p117 a' brown (IOY'R 5/g (lOYR 7/g} fin
<br />areas of this ]and trey smI mater7al a e ot7nd or are in7gstrea kg ~' friable; ca7car ansa moist; a
<br />"hat industrial develo type are 7ve]] m places. 3lanv C2 bonndarr modern rely ~
<br />rn sititecl to °a-23 to atkaune; agredua~t
<br />ping use for thane pur oses,tho7rete bra • housino• ~ •
<br />3 location. Prior Or 39 inches, light yenowish-
<br />rial Slt°ll]d p to mom[ fine sand light olive brown raven
<br />be determined b + the stability pf massive (2.SY
<br />soil particles. The ecause of s]ope or lack o{he soils rains tame hard, friable: (2.5Y 5/g)
<br />to
<br />'n'n eapacrty for soils normally- binder moderates common, media calcareous ant
<br />foundstions low have ^pod bearino 8-30 inches, soft butkntine: clear, n'n m, Pr°mtnent ma
<br />ick, good nahlral drama slir7nk-s7v a inhibiting °.rbouaaary-
<br />,ale for buried a°a and a ]077. ell pt•opert7es, gray t10YR i/1); nonraRne-grained sandstone,
<br />t is waterar meta] p7Pe, hazard of hvclroh'sis Th careous in spots; ma careous, ease t
<br />e not suited b Pen ditches for trails 7ortino• Krayish ges from 2erateir alkaline. P mltdly
<br />ecause of ra e n horizon ran
<br />+utf bunt ^ m ustneas lawns and garde SePvould 1 ~ from to floe satn Pale brown ins crotorches in [bickness,
<br />from to ecn,re.
<br />Ken fr 4 thickness, hor;ao mp
<br />>ide are, sfiPh urea ckelbet~rave]tlpwhat cl bean o I ase It a be _p°ta 90oom o t s20n~n h in t -Aen[to to c acarrm i n ar
<br />and t P d and filled 7cith outside °sad mp Terr inches. es De th bedr eouages
<br />n developed for hontasites soil materials, 3r fine sand ock ran
<br />P•
<br />i(?0 s tit bilittbdtedp ~rarel Rreaks ranCe siteit free 7 11 [1ne, This shapecllareas that Y g ~ ~o' s1oP~nhnE slo
<br />y arou I ]arlr pen 17ei
<br />to This ., soil is in itr
<br />77Ct•r soi[ has a proftle ran,e from ~
<br />Y Series scribed as re that is simillr to 60 acres in
<br />irk thicker surface ]fly Ptatic-e for the series tba profile
<br />ey exce~ve~ rrv series consists of 7r mod the hazard of crater subsoil. S + but rt h.
<br />soils Y -drained nearly clLdrained to son7en-hAt a severe hazard 17siio-ce runoff is
<br />,m, on tiptands• These soils let-e] to r[y' slo inn- P h are m p otected ^ht' Soil bloc
<br />over sandstmte. sty°t7° n inv , un r
<br />n`" ,9andstone is£1tn2cl i loam p ~ in the subsoil small areas of soils areas. Included
<br />inches. ~ r material than this soil. that hat-e
<br />In a re depth of ? :)loch of this more .
<br />ca]careoas resentafire profile, the surface 1nt-er 0 to 40 nativa Q soil is cuitiTnted. Sma11 nreas ar
<br />ik. fine sand • morass- Qapabitity unit IVe..°.
<br />upper ~ ]onm 7s brocc-t7, Plains i:anta sitr;
<br />e' sandv toart of the subsoil is about o inches Terr tr•re planting ° 71onirrig~ated; Sa
<br />'n' m about 6 ' Hale-bro77n, thick. The This Y fine sandy loam, . ~ sititabilitr
<br />snbsnil is mehes thick ralcarenns fine soil has the 3 to 9 percent sto cup 3.
<br />ne about pate-br•o7vn, hi~hlt. calclat~lot~e7 part of the in shM1ries. Profile described as re pen Rev
<br />;t, 7 inchas thick. ne an ] rang uplands, in , Presentatice
<br />.a_ splotches The underlvinSoma Lime sandv loam nreas that
<br />fine sandv 7oa is risible as faint runoff is medium a from ?0 to .lp a are irre~
<br />m and Iin matrrial is vet,t- moderate. The anti the ores in size. Sur
<br />ri- Sand. It IS hie6ly ht ye17o7s'ish- Pale bro7rn bazar hazard of water
<br />streaks and mottles.ralrareous. and ]htnev~s Ioamt' fine Included in inn d of soil blocrino is seve erosio7
<br />m, sandstone fra Thts material visible as nrP1$• area few Pnrn2' in the steeper and re.
<br />ly of ah gments. Sandstone ~ enerall.Y contains and a small nreas of Tassel and ore brn
<br />out 3J inches, bedrock Mostfew sandstone outcrops. Ulm s
<br />es Terr is at n de th of this soi]
<br />m .Y soils absorb water ranidit•, P toeerasse cultivated. Slanv ol~1b-a crass. ~ few is°la
<br />n and the3Pacity is to7r- Parmenbilit_ i and the e ~a and are no7v used for o resee.
<br />entire of v s moderate) va71ab1 fields have been
<br />s 1 is suitable for Y weld, inu ~itabil7ity7gated: Sandy Plains rano• Capability t
<br />9 Representative profile of Terr plant roots. Terry. ;tree
<br />Percent t'fnun 3- „e site
<br />and 158 slopes, m an area p{'v fine sandy ]cam. , Tassel•Ulm Pln
<br />0 7,• 2 feet east of the ,crass, ~ ~ ~ to 1T'E)•-Phis complex lsom,Plex, 3 to 20 slo
<br />S•> R• 59 southwest cort7er of feet north characterized b slo rough uplanderareas. If
<br />~• ~ section 34 In man Y gently
<br />,~ to stron~,iy
<br />`~2-o to 5 inches, .Y placas the landscian
<br />brown (1oY of fine_grained s1o o ~, g,-
<br />brnw R a/3) fine sand a is datted~withp
<br />a t20YR 4/3) when sandy roam, Of dee AS Stone. There are ntcr
<br />attUCtur moist; dnrk PeT SOUS, StrAleS
<br />friable; emildly a16o single grain n lights arse, blocky shallow and moderns ell as 1on~ rides a and co
<br />R't boundary, aline; ralcareou y hard' °ery fine-grained Saridst N]y deep soils over i nd SlOryeg
<br />~S to lI s; clenq smooth Terry soils one and sandy shale, nterbedded sr
<br />Inches, Paie•brown {lOYR 6/3) line sand ~~ ake n percent ~
<br />dark brown (IOYR #/3 Tassel soils, , n about 5n
<br />crate, medium, ) n'hen moist; weak y loam, Inchtded parCent+ and I71m soils, n of Ehis comp6
<br />to moderate, prismatic structure to mow- pn rids in manpina earl
<br />sti htI nteclinm, snbanKUlar bioci~inK to weak small „es and slo ° are a fen' small remnants of Io
<br />g y hard, Prirtble; thin y strttetUte; areas of Pen, Sofne Sandstone Ott tefO S
<br />bound s' calcareous; mild) Pa tehy clay Sims on totes I'°amy All P > and
<br />a wry. y alkal;ne: clear, Terry gne sand uvia] land, ~
<br />~a0-rs_„¢ smonu7 taon~ slo has tn~ 1 of the more month btt~ommor
<br />pen. Ta fine sandy Ioam is close to a
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