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near] lY hard as it dri 52fRv
<br />f. Y vertical bank. eS' TT'hen dr, gofL E
<br />Ire sail is suitable IoC1•meabilit Y, these , hold a Y
<br />e for S' is !.a soils
<br />aePt~sentative Profile plant roots, pid> aitd the Colb}' soils
<br />crate a
<br />an 30 feed Wiest o an a ea of land Ioamt. sand 3 to a'•ailaai d~th~erbcaP citytes h ~~ moderate rate
<br />T• 1 S., $. 5g f 6he northeastra~' h~00 feet ~ $ePresentativeltth"e soil h• Pct•mcabiiity' Islm~'
<br />ver ~ • corner south is suitable ~ e
<br />cD
<br />AI-a to s ;o es, srayisD. °f section 2, Sce~ofln a Cultivated le of Colby loafor plant roo od-
<br />frfabie;nne, SranuhsDrottn tioXR 3/2) loamy sans xp-•~otollsastcotneroflsect o~ 3eet south a°d p90rcent
<br />AC--S to 9 fnchesut~l t clear, sinoohme; slfgDftyn'hardmoist ~ llblinc}/,3 brown Y C' T, 3 S•, $. 88 feet
<br />8ular moi saad e; so
<br />ab can 1e(IOl bkoci y}ns b~°kR Sty.') erpam ea dark alkatin strucft, rs er afeia~RtO /~'eaA Pfine ° a°g
<br />CT-g to IO inches 1' cleaq smootDre• rely hard,h• medtnn, CICa~O 20 I3 in abrupt. smootD ble; calcareous; g~aulat
<br />fri /3
<br />C~- for Qpe if ae R dro,grad enpR n/3)n asamy sandr~lark 6 ~ kr; structurehe~tbuoist~i,vea ~ roars Io m~Dromn
<br />15 utral; moist-
<br />friawn f10i' a14~3'bro,hvq~ (70~ R boo) da s rc dark C?_ t~r~rotrhes atmo<lera [ej is en inaeed~ aadable, eaksra0fua
<br />ble; neutr ) n~ a m 0/3 sand, 23 y a[kalia to str
<br />The A rizon Sraduat, smooth mass[re; bard, flpd8 inches time- clear, smooth ~ and
<br />6ro,v
<br />Th$Iakelandh°m mYrsand f rain°abeit s trfsdbb~hes ry rk smabe ~ ncateounD tom ~e1 r~As, a/3)slioaa', Drowd-
<br />IOa 6 Sra f° thf x-23 to a0 iurh dart'- s, a1O atelr alkaline htfy ham
<br />soil is pn . 3 to g n in
<br />represen uplands. It Percent s1 color, bro,rn ~• at -b g a
<br />tativ has (201'@ 5/iron a (IOSR s B ~ 1 $umal,
<br />to slow, e for the the profile oPeg f8oD1,~ bard, friable ) uheu mni )One sand
<br />The hazard set It g" Surface descried as fICi~;~,aboupt, smnot4~bouolcareo mass(re~
<br />areas of this
<br />rat of soil runoff is me GO d1ry, ns' n,odera~e~y 8hght7y
<br />ed fields tl all are used for rau„ t rag is sec-ere. diunt sandy etay~cf eS, IfgDt Sr11°n , alkaftae;
<br />nortirrigat Eda6le f rlaculkienrionseeded to agrass. old ct ]tic nikaltnen'ussi~rra Latd,firU~t Dro,rrbrf101'R 3/4R B/4)
<br />abilit Deep Saad Capabrlit The soil The A hnri, calcareous; mo) when
<br />Y g'rou raA~ ~ y unit _ from LOn ran deratef
<br />10 $lakeland Truckfo ae site, t!•ee planting s tit- Dro"r'3laocolorrDes in th cknessoarn to revs On y
<br />Y sand, 3 to ,ry association mo2bf loam The IIC horizon is°d ff~bE tayish ndy foam,
<br />eat. of this oclatiotn, s1o kcslBUl.-Blakeland fro uplands. T]~e a° a~ Percent glop sent fa som brown to
<br />dune age leg' a places,
<br />tckton relief, though it a It~ls ~ i! p_ at Icast 60 eti' acres t are itrenul 1•-This Soil is
<br />20 to IO loanav Iso rs on lono- 11.E 72i areas of °~ is rapid, , o about 100 ar i12 sha e a!t
<br />acr
<br />percent of Ind
<br />sand, 3 to 9 percent . nano„' rid e!'osion are the hazard- es in size, auge
<br />has the more n mapped are, slopes. nlakesgu~~ ntr sP1'ere ' ' of soil I I Sur ~cer
<br />Iac1u ycutle stn as. It is de e some small t!r!l>rote area ' °,rin vrun-
<br />l ~ ar ctcd ,
<br />loam - ded ill mnppino-peS• Pressional or half Il ar of _
<br />s Inchuiedii
<br />3bouC acrcn`sso ld n Ioant. maajer
<br />en n
<br />} sand and I*Oamr alhly~ale small are. about half is the
<br />The hazard of soil tL as of ~ralent tart of tar e tr =mass. The cults.soil led
<br />it is ver to blo,ri lan is eultit,a
<br />rained. SmallePe Places ifgcjcr'crally is modernt • at:~obcen~,~bf~rnling ol~rations andiareas nie niostld
<br />equate col>C3, e but ur it ab, ~denn 1Fe[Q soil. fat•med ,ritlt
<br />blotring and areas hall berm is not main- t-Ie-g andoncd and rrseeded to „ fields
<br />This small blo,routs severely aff tlautinn ° lronh'r•igate Slo ~ Jtat2t" odd
<br />association hate fo ~ ected 6}• soil 1 b snitabi]ify-„• d' joamc. rnss• Canbtlit•
<br />mapped gill Is used for, tined in places. alattp 1• I es l:an„ 3
<br />Consegnentl Y in areas that ranneland and ryas CoRO ~e site; tree
<br />The }, all areas exceed I00 D8 'Se17eS
<br />soils are hire a acres in siz
<br />nail ple ~ not suitable for cuitivationnativ~ ,,. ~' TIIe IJacono
<br />lantinn nonit•rigated. tlnss, lcrel soils series consists
<br />on
<br />p d suitability ^rou ~ Deep San I c C.a mbi&t • riutt2 that o}. terra of e•
<br />o p 3• d rai ~ site; tree In a r. crlics sandTl'ese soils forl~ed i nllo,~rt nearly
<br />Colby Sel'les brow epresentative }' and gra2'elh-. Y allu-
<br />n and Profile, the e l ~'eallma
<br />tine" dark n,,a .. sarfac serials.
<br />The Colb " k• It is nonca] ° }rsh-brbx•u I s ra
<br />is
<br />loliina Y series consists ~'rarish_ car•eous_ The oar t abbot Y h-
<br />Is
<br />a to sty of ti. brgjr )
<br />tr'med O71glY sIo ell-drained. calcareous. n cia}• about upper part of thg Inches
<br />in mind-d Ping soils on upland , inodel'atelT; ish-~,ra}' sandte loft-er 'art $ Inches e subsoil
<br />I!t a I'etres ep°sited Loam , s These calca • 1 of the sobs thick, It
<br />I entativ profile S material. soils teous c1a}• loam about oil is light Ig non-
<br />a!n about e ,the splotche 'and ntueh of .5 inches br0tvn-
<br />~'er is ta1~ Inches thick. surface Iairf. ' n s The underl . the lime thick It is
<br />1 e•bro,r , It is cal , rs 6!"o,cr2 bout ?? inches, }!rt° material I' risible n
<br />'hes thick n, highly calcareoust ~ us• The coarse The u> heRins ,
<br />This nett sandi s II'hite
<br />hes, by pale- is under gam talus , b clac nt aiitper art enlcnreot>sde>th
<br />bro,rrt 1}ucalo a depth Y~~ttt56 1 a of 3~ pelloa fine ,.anise loan?t- sand that of
<br />> Iliohl • I of , a cIe rtL cent bromn
<br />~~Y calcareous Sa~dinches !s light ns Ionrn• Betmecn l!^]tt-brbtcn salldrehes• the and meduun o •, con-
<br />} cla - ,Ycilotrisli_ Dacon and unddrh"irrm 5iacel- 13alow
<br />y loafn. brouvr, mater r, I soils absorG i~atelelsion~ly, ands theirr, s ~~
<br />soils a tacit • a nmtlel'afe.
<br />are suitable for roots to Pcrnleabilit- atailable
<br />a depth of b Is slott•. The
<br />out 2¢ inc
<br />hes.
<br />~i;
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