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<br /> SOIL S"I1Vt.Y
<br /> Ic:e soils are um-d for pasture, bouirsites, and indus• Id„udi,h-bra} -rrvrliv salul. In the sill facts Ltc.•r and
<br /> sites. ill:ticrial Soil n`:u-tir,n i< nn+d, ralvir :ell:alit-.^,
<br /> ninike plutilr r,f I.nn_nlnnt rlay. n to 3 pr•1r.nt and io flit- ,tlh-Iral[ilia it is luildly a11..Iline. In Iuo-1 a:v.:s,
<br /> taled 110 fret ❑,nth null lnrl rvof wv,i of Ihesmitlt gypsum rl;v.,lals and soft little x•�n•;-;atirn:. : Iv pre..ut in
<br /> ccof5 cc. 13,T.-2 \„ R. 70 W.: Our laver:..
<br /> 11-0 in d iltrhra, li_Lr I,r„e ui-L _rah' 1_:%1' r.;_1 rla)'. Frnc• I.Ovelnml �nili have aintlel'atC pe1'n a':dalll l'. .\%'nil. h c
<br /> Ish brown (S:%Y di'-') %%L•,•n utonl: we.ik. nu.linnl, watI-t•ra pas ltt' for till• pro ilr L+uuu I.-I al,• to I. dv.pvnsl-
<br /> suban_ular Idnc%F Flruentre: hard. first%: valcarcuus: ins upon the th-pth tit very gl avclly maid. huo;a can pe ^n -
<br /> strong Iy:Il lalir„•: char•sat ill, 1,1•„undary. trale to a ale,lit Of GO inc6r, or Inure, anti the iensun.d
<br /> It!--S to 21 iiclivs. li;:!1; rdirrhr,mit (1110 5,011 ,•hL olive
<br /> brown (7.517 •1/3) whra n,ui,t: weak, cnano. suban• high w:list•tahleisat:ulcpthttf'_tri l feet,
<br /> gular blocky structurt.: estnuu•ly hard. ecr3• liens: •111eie soil., air used for It:1-11111`and crop;. In ,Dine arvai
<br /> ca a lcar ,us;sln.r.gic alkabm•:difru•v bolmilary, tile%• am a source Of; VaVc fat'roust 1 1:6011.
<br /> coca-21 to 31 inche<. tizht ,.her-hrown t_.-W 5/3) clay liopreh•nia6ve pr01il'. of LOrelaud Clary lualu.,1(0I pt•e•
<br /> Willi many, tuc•tima. di_tinet )ellowi,h hrn+%n Uu1'11 - I
<br /> L -l) utilities, dark _r:gisl, Iwoual ct•ut ;lu res, m :ill :u'ca of f.ut'el:uul :nil, loc tied 71) feet east
<br /> rnolht; Inns ice: extfe::rly hard. eery ;inn: caleare- a11(1 ':;11) fret soot) of the unrth+ce,t euruer Of ae\0.� ill I.
<br /> one; con:sImm Win to medlum clnsrcrs of _31,stun 2 N., lt-fa \\•.: ` aa-tj 04s/1 VN% 1\
<br /> tions;crystals and .'r:. laii In medium, hint lime boundary.
<br /> .111-0 to 11 inCLCs, dnrk grayiMi brn+ru 001-It 112) lic .t M�
<br /> tirnl5; stron_I)' .dka;inr; _r,dual, dilru•e hnundary.
<br /> c.+cag-31 to Go lushes. ;n:c-mire (%Y 13/3) clay will, Costs- clay lu:uu, ver3 dare: hrnwu IJOYlt :%h tt hen 0u.i•-_ `
<br /> olon. Iaeditua• di:lino Mire (5Y d!:) rumtics, ., ivp nlodcraie, line and mcdinm. I:r:unll..r s:rufture; e•,.I, I
<br /> MY 5/3l +nUu LloiW n "mr; exlrrnle;y hard, eery very friable: ealcarvous; m.,dentell all:aliuc; cleat:,
<br /> firm; enlcarcol.c: corona. fine to m,diunl clusters smooth boundary.
<br /> of r3'p;uut cry/ fal• and tc+v b, c',nmNnl, line and pro• AI2-11 to 20 inches• dark grayish brown (IOYR i/n_) li_!a
<br /> Muni, hunt live coucrriiuu.: uludcr.ucly alkaline. clay loam with cummnn• inedium, diiourt )alin,u.h-
<br /> brown (lOYR 5/4) nndnrx, eery d.rat Srnon 1191it
<br /> one Al horizon nn2t� f:oru 12 to 21 inches in thickness and 2/_) when moist; weak. nu•diuut, rul•atculnr bh+6y
<br /> m clay Inam to May or +iity clay in u•xnrre. Tate C horiznu structure; hard, firm; ealcnrcous; modcaawly
<br /> iges froth heavy clay Irram to clap in texture. lu insist places )tile: abrupt, sntooth I..runda y.
<br /> de is at a dgWh of mom slain GO iurhrs, but in a fete areas Clesca-70 to 30 iorhas, pea vislrLrowa HOW 312) right clay
<br /> is I, vren depths of Q and Cu indu,s, loam with cowmun• uu,liuut, thitiuea, yctlowirh hrnau
<br /> gmant clap, 0 t0 Z percent sWpeS Rem.—This (SOYIt 5/4 nod GIG) ninUes, dark aramb prom.
<br /> Ill the CasICI'll )a rI nI IIIC Alen. _\ fC%+' SOIL areas (10Yft 4/'S) whru abort; m sMm; h.,rd. fria Ll•_;
<br /> 1 strml_Iy ralc:ur,.u,: fell In i.m nnr,•a, n1.,• n,
<br /> nrwhat Concave. In npst places this=oil is in ire^u• dules of y um et- sd_ a d iwr„n. mcdir.:n
<br /> 'F Inner than 20av"A In Ewe. stud coar£e. `oft +chits lilt.. >cCrr;:a:iollo; ❑bdcrale:).
<br /> •d %vit.fl this >0i1 in lnappin= is a I.oil•'nlnnt-like nfkaliuv:clear, wit I...Iond:,.
<br /> I IIC2- 30 to Go inch,>, light I•ru-null, drat UIY I: .r^'y +.-
<br /> 11.1: c,lnlC :II a lid l'dh of Ir�S lily6 -I I) lathes. ,11Fo _nosily stud w-llh ncuty. I::ellinnl (�i i.�incf. .•Ins:_.
<br /> •d nrd small areas of C. IQ UK clay loanq fret, brtvn (..51It :/(;) m,:plc•. ;;rat i_h I.r.,w❑ ']U111
<br /> percv:ft ;lopes; and Finn Il alias Cf Ireldt clay, 0 to %/-) when Inni�f : mot:le pea:ut+l; Ir.u.e ,Wien dry aril
<br /> ant slopes. These MI AMI soils uln!ce up about 10 mom: u3my all shut.
<br /> Of earlf mapped area. The A hori.nn ranges from 1S to 23 inchet fit this::ur>. and
<br /> lost plaices runolr Is Flow. but soluC cotrraee ,leas train %andy clay 10nm to Ony input in texture. The C hMina
<br /> raugci hour loam to clay Imin or sandy Op Mmi in fex:uv.
<br /> tiled. The crosion hazard is slight. Dlainnge and Deldh to undedging ,and or gravel range, tram 20 to su
<br /> I of sail and nikali arc diflicult because Illis_soil is incites.
<br /> orI311oft Loeelnud soils (0 10 1 percent slopes) (Ill.—These soils
<br /> C nli 0f the acrca^c of this soil i;in pasture,except cur on Fhranf terraces anti bort0ms m the enstern pnit of
<br /> m arr.0 that arc urbanized. Lffors to cstnblisii the .1ren. !if most places they aim in ilTegidar wrens nitre
<br /> .l
<br /> stands Of ;sass nve Leon partly sacCuSaful• than30acrr;inslze.
<br /> silty unit nonirrigatcd; Ucc suitability 'I he profile of We soil., Is slllydar t0 themir described a;
<br /> rcpreseutalivt- for talc scvir;.but the texture of the surface
<br /> laver rnn_cs frain Fundy clay loam to clay 10:1111.
<br /> ant) Series Included with Ihese soils in mapping is a I.oveInvid-like
<br /> Lot'rland sn'irs is madc up of deep, somewhat coil that Las a li_Act- colored surface Inver. ,Uso ins uAd
<br /> drained soils. These Foils foinlerl I,n Irrraces and °arc gravel bars less thnn 1 acre in size, small arras of �
<br /> lnnds in loalnv lallnviuul that ( rc'1'IiC., r`11mjI3 clu ledi soils ay Win,
<br /> iu%clid areas of -Ni about soils.
<br /> 11s 1 het c in- tr
<br /> tly materials. Slopes arc 0 to 1 lcret-nl. lilcvatiolls
<br /> )0 to 5,700 feet_ Ti:c native vt,_etalirua is mainly c eah nrapprd nnr:t.
<br /> s and Line craula. Annual )uecipilation is lo_ t0 Lunod is slow on these coils. The crosion hazard is
<br /> cs. %loan cnlinal air teulper:unre IN .IS= to 53 h° ,, 'lieht.
<br /> frost-wereas0n is:Ibont 1d010 155 'Inc., \II of the aloe(a a tilt-<r soils is used for in•i!'atce t7
<br /> Irprc::nc:aicc pro;sic [lie surface 1:r1'cr is calcar- suicrotability
<br /> or ygloup (Capability unit IIIxv-1, irrigated; lice o
<br /> lilt glayi,h-brown Ligl:t clay loans about 0-0 inches ylulability group s)
<br /> !t is n;nt:led in t!IC %%cr pnit. The undellvin_
<br /> 1 nbdnt 10 inches thick, is St on"Iv rnlval'ccu1' Made Liz
<br /> ')lull❑ ll••!It el.ty lOnlll that is uud11'ed. Undi•rly- Arndr land Taal is on treat Iv level arras alms^ St. Frain
<br /> 1 to a depth of GO inches or ruoro is n1wilad, light C+eck near the ca:aern edge of the Atr:t. This land .5
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