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<br />Altkoug{t !Leer Boils 4rpitally are t-Ieareotu throughout,
<br />!tole upt~moet ten rnrLm U noncolaraotn ht mms
<br />plncee, The degree of and depth to stntiRnarion vnrryy
<br />with~V, but tln !extort ie domitrntyty lane from • deptA
<br />of about B to x deMh of 3p invltea The depth ro mattltng
<br />mn,¢ea tyt to 18 to IIO itteltes
<br />Lrttalmpnlytto eo[h an aatser axtuted, an log mtl
<br />drnhted, and here n darker colored mrfate layer tMn
<br />lifllhrfp Boil!! which thgy ndjoiu in many plaaa Un-
<br />caapaliQtn Bak treeltebk ()e+de mile lest hare a tioher
<br />colas! atrlaa layer Wort are lea we0 drttitted. Deatn•
<br />ago is amparabte to that of RMt~yott toils, but Utnvtu~
<br />pallggtro~ mica sat conger tavtuted, lmre a darker stored
<br />nerfaa la)•er and trek tln narumuhtioas of silimte
<br />else typist o~ IIlntuon mite
<br />In !!tale utgerni aorta, UnrompaltgR mile neppott n
<br />thvtve ester of gran, trillotq mtd teulinueod. llta trotee
<br />table, whirl! b high rte. lout part of etroh .ear, harms
<br />rmin iu souro plates, \et~ertlrokn, !hex mib ore mod,
<br />sorely prahtMitc mul me used for celery and many
<br />atrer crops,
<br />uneompahgre ~elay bem (o to n ~ettan alopaa) tutl•-
<br />Tltia ail is ou Nood pkim mtd Iow tatracea Stapt
<br />[or the carfare !Beyer, tiff proRls b similar to rtes owe
<br />deecrtbed an !,epics! of the Uuconytahgro aeries. Tln
<br />Intyert aateage bordee Ns UneanpaltFre Ritar.
<br />'Chia ail mppoMO n good cover of nxtiva ranm, roil,
<br />lows, alai satttered eouanarad. It stn 1w tilled suootn•
<br />ftdly Intt aitathl bs nrttRcially Ilrai+ntl Oemtne tltt rooter
<br />table is h~It nt more 11n~riod nearly every year. This soil
<br />k not highly elttxeptibla to erosisnt bat occssionnlly it b
<br />flooded and teeeire^ depoairs of net. (CxpaLiliq• unit
<br />i-Iw~taaeirrigated:L[a+1 ierigaml)
<br />Uat~t Where clay lose, wet (0 to R (,erteut sbl+e~)
<br />a~l ie uee~mnat ofetlt~a,yeae~ Eiso l~r[or !hoe lw'r[aa
<br />Inter the ~ueflb k similar to tlro one deacrtbed ns ty d-
<br />eal oaf the l:tvtantmhgre. aarie+, but ail )ayyeenn geneca~ty
<br />me urottled. All flu scrooge bottbrs the IInootnpahgre
<br />River.
<br />Thb soil mpppe~e n fnir.roser of watenrnkrnnt gram
<br />and willow mtd is ufed primarily m ratite mnga mid
<br />for uathe lay. It ie ua attitnbk Roe tilldl crop! nnte$
<br />artifkinllr dtafnhi, It is trot highly ataotptibk ro eto-
<br />eiat. (Gymbili~r anti V[tr9 teottievigated; IIIw-I
<br />ire~~atttttd)
<br />Unrmnpahgn one candy Ioam (0 to n petceutt slopes)
<br />NtJ.-Thiamil kon flood plains and tow terraces RattPt
<br />toe rho otrrtaoe layety tltt proRb fa similar to utt one
<br />described as RIpicn1 0[ flu Unrnmiahgro eerier, Moat
<br />of tItt acvatge Wnkn the Utroompalrga IGten
<br />Tleb soil sappoeta a fair cover of willow aced gores
<br />It nn b used lot, tflled cmpq Intl the tenter tnhk sno
<br />en,tee and nt Wme lima of Un ysnr h rune enough to
<br />the mrince m W damaginq so ecopa This Bolt is mod-
<br />erntelr etraceptibh eo wind erosion. (Cnpnbil{q met
<br />Vlvr.,4 trartirrigatad; IIw-I irrigated)
<br />Uaeoep~t~~ gtn.elly loam (0 b s poecent elo
<br />tUn1.-Thln sw1 ge!wta117r is on thox ports of eke tlo~
<br />Phln neaten rho atom hares Rivee and f]toeo adjacent
<br />tR+ldermi~lnr to des amydesceibed aimrel. It tors n pia
<br />aeepahgre wdar, but the arrtaro typbal of rtes Urt•
<br />rnrt ~~' 14tet' b le to cep per
<br />art-oa-~r....-a
<br />'l7tb soil wpportt x good noire rover of gran, roil,
<br />bw, and atatteted oatootrotd. TM gravel in the our
<br />taoe byte i~ hard on farm ttntddnery sad otnM titlaga
<br />di~cuh unlaae tM lntger pixy ate temorod, ldeeause
<br />of the grerel this edit n somanint lea relwbk m~.rot.
<br />land !Lon alher UtroanppooAAggrota mib, It b trot higitl
<br />aalee bb to erosion. (Uayxibilily unit CIw-g nont~
<br />g+eted; Ilse-1 irnguled)
<br />Unoonpahrte Iwm (0 to 2 txt•rmt slata+) NN: -27+ia
<br />mil b en flool pbiue and low hrmora It tens appmRls
<br />similar ro tltt Im dcverilttat as !epics! of Utt IInoom-
<br />paAgte oetira alaK meat Wta(er tlso UucominltRte
<br />ter.
<br />Thb Boil tuppatn a goal R0.tite toter of gca~, wil-
<br />low, and sattaed aottonweal. It mn I,e nanf for tilled
<br />crops, tart the water table fl,uxttum and gettetnily is
<br />tte:tr enough to flue nreha at sane part of tl+a year to
<br />eaux Ilamape to erorol1ac This soil b trot Lit,.ltly etnceptibla
<br />to etooiay n+t noaling and deposition e[ at16 art tom-
<br />t~~ Ate) (('.A)altllhty llllh CIw-~ nallRl~atdl; Iia•-1 irti-
<br />Untomptthgee lanes, pet (0 to S )>rroent slgxs) (ua•I.-
<br />17tb soil is m sli t depeeniau at flood plains Bad
<br />low terraces It lies a lxoRk aimitir ro Utt one de-
<br />acribel as ty`(>ical o[ tlta Uacompabgte eeriee, alwt
<br />nteaa border 4n Uttoompnhgee River.
<br />'1'Itb soil mppoAS n fair Bore o! wamr•loknnt gauss
<br />willow, and aalloted cottonuocd. It is iilely to be
<br />leatdetl for long periods, amt rtes !rater table n xt or
<br />near the aterfax mach of tla year; coneegnentiv, it b
<br />+rot a+eitaWo tar tilted saps unike~nn attitxixl~y 1(nined.
<br />This soil is ttx hi~blp sttstrya.ible to eroatay but it b
<br />mbject to flaali~n~ qq and ailtatita,. ICalwielih• an(t t'Iw-?
<br />naurtrgatnl; IiIw-y irrigsm{)
<br />Vernal Belies
<br />The mile of tltt ~'cnul arras aro deep, sail drobted,
<br />rtttJ nualcmtely Rttt tcatuteal. Th~v are Qsaseistd soot
<br />that formed on serenm tetraon m tair(y mifatm, cal,
<br />cateoas tnalerial etalkrliin br clean tared and gesvt0.
<br />Soib of this atria ate maletately extemite in tlro Arta,
<br />muin~v at tla edges of the telb;v of tltt linaatpaltgte
<br />Ricer, aautlt utd !ten of the loon of I[ontertse.
<br />\'etmml soils 0.!.e a light-0rown to inborn, friablq
<br />granular awtatt !aver ~ l0 3 inches [Lick. T1tev have
<br />a nrodetately !tali tlardoptd, brown or taklbfi~rown
<br />subsoil !tent b modemte~v nos teawaad amt ltaa pris-
<br />matic amt blettdty stnrrtata The snhWatam, whirls Ire
<br />gins LS h 30 i+tcltea below the wr[xcq is 1'
<br />eokateotts, loose soot and greteL Aaumakttioas at
<br />xromlary aktinm arbarate Ixxur in the borer tart of
<br />the subsoil utd rtes upper pan of the subtingtm. The
<br />deMlt to bedrock adinxrity ie UO i+a;aes or moss
<br />tea aoib an not highly tusaptibN to acotieu. The
<br />~eg•utro matter eauent n trrodetat4 and tM atructote b
<br />Tbbvhhptml ptetRb of a Vernal sail, o+tsfaurth miN asst
<br />and d00 het trosth of Nor antthaest cpaer of sec. 17,
<br />T. W N., R.8 W. (lfatttoaCoonty)
<br />at-o n + tame, too; oast news (tAYa Wit aitta
<br />Oq, arewn es Bata atawn IrdrR e/il ware tpaalrRt~r:
<br />rtr~rtet.. nNals wM oedw~aoaukatrsa,' PH t2;
<br />are1w1, assota aaaaetq.
<br />Colons Pit November 06 I-5
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