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23
<br />sandy foam,
<br />pnAM6 CQ~Ty' CALOrip4O to 18 l0yR~5p3)ea+kt~,njCtnreY h~ ~areousto han n~
<br />n3t~-_. i,r°a.'n 'Tar b\oeK~~s oP Pcds'~oaergtC\Y
<br />m Place to suban~tchY clay int sFtOtoUes; ~ j37 gne sands
<br />live
<br />fco el tbin P is fs UounaatY- loYft mac
<br />Varies lop ETCent~ raaua~, sm rerY Fnte 5131 and e° yniooth
<br />C layer - calcaTreOUSa ~ on~ tot $0 p ,d ~° gin dim Cb~ t 1TOYR bcown~us morstua ins iime
<br />~ snif~. laces iS Tango ftatn the soils aie pr G14ay1S1oam, Utown friable: cai~ikabae; grad (~^5Y s141
<br />and lII ~ nOeS and but lion stTghtlp Uard,moderatet9 hen
<br />n short stated for gra2tn~ble far cuttiva in stee9k5; eno°nag br ~25'I 5j4na c°n-
<br />a arllo , °t lap n~ being mined fm- 3°to ag9r inch pa. tght o~ ~Ute°wcatcatm ~entan'°ttles:
<br />a~~slia w r far
<br />snag°ment. is TaPid~ot usable f a or ai'° c~a- 2 loamy aaas~ve; i'~on, meainw.~nnaar estane. ttgnt
<br />grate this land type fter is pun arty most; com eacgwzvYamea c~ee aty rat-
<br />ng t ~;
<br />d lherea dump'°~ ~ laces.. tarns tame ' ~t~attoe . ~t n •~
<br />luau °f ravel, an used as a taetal m P mg °C moaetatelY a rnhthlang ns,tinc.
<br />nd ~ 1tOg5 . ft but - n0ncalcatealKa thicknes<, ftoID
<br />~' Sfil ed ~ had Ypesarehi ehwayited mono pt~e so} s ft~3y in~rav ~° na Wes) '`n0a2 toes iacn~ d°ft0sn toanrang s
<br />:ck thts la ~ oT g a stabillac °f btndng eb~zon rangzsbcOW '° cierTae 8 UT~ans mstetiat
<br />ever, th k beac , a~nsm in tegtueFt t atcak rang from
<br />ddus LTr Fat"c
<br />Caas tCl&l fdSe p On _ lbe~at rim O ally pha'Qa 11°aPr0110Ct1as9 g A4Ss1i brb°p SanaY in thic es~<. Fth ° b C
<br />Tse for Fe doter o soils rip a shrtnk-srd of hydrOl9s sand ~ to 24 inches20 inch ~ open 11eB1• u
<br />sllouldaTticles. ~ ndations, lO :l~itellesafor tralu5p°rting Lrome° fromtie~o t g ereettso~ is iu ~rt~ e.
<br />~~papnatfor arainp p+ aTp~f rapid~Pa~ixld have ~ ~ ~ Y¢0 e :.andY loam, dntlV s~ p~Ogto BO aoretio6le d°'
<br />ut db~ and arty at
<br />fo°rab Ted ~e>ite was a d R in~ from oGheas aum4 .Fh STne had ire so het t~.hant istomilSeYtes,tbup ttihas w,
<br />`° ~ r some°areas~tter ~Tl n~ have bed ~ij tnatariale, laclY shal has a pr t tativa for t1T ~urfacht So~ blowing
<br />ill up, using old gravel p wttl+ ~ PL unit VLt `his ro as fac teseer and Subso'o id51a Qas. Xnmorea lay
<br />e
<br />b° d and filled ability lauting ribed stir ay
<br />tree F 1 ra
<br />fn so sites. rte; thtcker hazard of wale o
<br />ine a`-eas~l`eod for h°tn ranffie s ' and the in u° o~ S ill
<br />t14an p the , ha
<br />ks re bazar av .
<br />areas, dyvalop a] Brea d s - areas e in
<br />d then, d. Cxrav is a seve ate small area soi; y
<br />rigated; an
<br />atR th ; to 5 n
<br />3, nonirrT$ roue 4• cnapPtn~tbsoil than it is C'u ti 'V boa
<br />roue TeD1r
<br />sutlabihty g °mewhat in teach °f this sn
<br />- cd t° s ing bility unit. suit.a, ilttys open 1. for
<br />Series lists of we11-a J 'Strongly n atrial yz call: GaPa'roe Pla°ttn€ 9 percent rasent?ttve
<br />anti g ~, Site; m, 3 t° as rep uregular
<br />~ The'~errydratnedotnFa5oi1s1focmeddepthaoY~ to 40 plains r~fina sthdprofi`ana~in a e&5 th~inare Surf~oe
<br />aco~water erosio t
<br />ds. Thes " is al TerTY s
<br />Th , Yt is ou uP 20 h 4D
<br />tvelu lan Sands' is br°`vn' is sod h
<br />ogcess one lager to ttga
<br />soils onndst°ue. thy surface es thick. Tl ' the $er1eaand to f d thy azar ing i5 ~ e ore hrokaTi
<br />°vec ~ rofile, about 5 inch alaareotts tth° in shams medium, and of soil b ateyner an nd j71m sails
<br />inches• rysentative ploam brown, art, of runoff The haz to the ~ Tassel a
<br />cslca c ~ t of the auhnc ter, thick. ~~reausr sa°da fait n'°~ eluded Ln map!'~lall areas of ~ fe n is°eed a
<br />u ab htg y Ls tblealy brown s ara asantlstona outt~°native Ora haveyb~bihtV unit
<br />loam ant Fwn h1Y llm vts P na area ,
<br />saRdY• i5 pale-bro. Some is very fi an a few °tl is an d fiyrazutbx-- ('aP lree plartti;
<br />Tl inohes thick• inn rtaish-b n loviitble as mast of thls s d- 2a'1ns ~o~Pr ~ rangy site;
<br />sabso 7 mate rav+ - ltivate
<br />about y tindand ~l~~s ouslo zial lt~e arallYt cO depth to crass a°;ar~gatedw~aAdg plains to 20 peTnreasS17p0 s
<br />fine~sandvslOh ~h1a This mate bedCPak is a
<br />in~~ n hll sael--flan eOrapler < 3 t npongd sl° to~tcrops
<br />sand. hand mottle gandstony \able sutra lm ougl 1 P
<br />streaks idly, modz at lyarapid, Terr~h a complently sloping t°'aotted aleshand rovof
<br />sandslOIIy39 inche rb water ran S~EI f by ~ scan sw es
<br />ibty is 3 to 1
<br />of ab°nt ors. ar<TCterized s nd ,
<br />abslow permeafac PlaIIt toandy tQanl' °rth Tn ma'tt' {?lane sa store .as 1oi ~aridg~~tetbedded saft
<br />Terry Soils
<br />a a,ctty s sltitablTerry fine sa 200 feet " °,4, of fine-°ratned as xvelldeeCi soils 51m1e. °mPlex>
<br />watez ~ entire soil i_ rle °f rays, " ction ~ er sods.
<br />the rafan of gt c of sy' of dow end nTOadston nand ~ 50 P°rCenl p<tt Y 20 per;o
<br />t1Va a
<br />and nta~ are< ocher sha
<br />~aprsa slopys~ t ~ Sauthwe. T°am. lned sa u abou sPt15, n ` nts of
<br />the • rx
<br />9 Percent, t ° One ganaY ~ hl~kY Erne-ei'a ,ails maka nt, and f n' Sma11 tenln s and some,
<br />and 15fl ~eri9 ~.: n tl°vft 5~,osst: weak. coahaca: very `Seery ' g0 peting a~a d outcrop ' rro
<br />Yn 1 spits. anP are stone c
<br />Q S•, brow ien slightly tb ally e5, me ~, na 1
<br />7' p1_A to 5 ins ~iovft 4J31to s;nBte graini~ous: near, srnao T ylnded in in slop so vta la°d~ the tDng'+ in
<br />stzactuce~~atYgatkatine: c4tca 31 8ne Banat Tm d- p6 4laareast°f sandyy toainy rnoretsmpOtt4b~lose. too&
<br />friable, Nn (10Sit bl k 1, gm< ~ h y O
<br />ny sand
<br />than
<br />b°nndar9• ah. Urft°4~31 .vUen m°ist: wen
<br />re Farting C.o wen" Tee a
<br />Structure, n as
<br />yl fi
<br />to T1 inches. Ft10Y StruCtu a,es d° SSe
<br />Ta
<br />iZatj5 nark brownnm, Frrsutatis banfi°tar ~ a3 brats ° sm°ottt gkrong 610[105•
<br />ed rum. atchY cleat
<br />eiate^ m line;
<br />to n1°derate, m~bte; tai
<br />sliShtl9 hard, ~ : milat9 atka
<br />of Pals ~ catcare°
<br />boundar9
<br />~~
<br />464-3a0 -74
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