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<br />F:1. 1',\tiU t'11h\T1' ,\L'IL\, r'uL[lll.\11(1
<br />mat' 111• nrrdoll to issuer su rrita 1. 'I'rel•s lh:d :u•r best
<br />suill•II :uul have 1!uoll sln•vival :n•e Corky \luunlain ,ju-
<br />uiprr, ra =uu•n redceJ:u•, ponderosa pino, :nnl Sibrri:m rlnl.
<br />~hrnbs that :u-r best suitod :n•r skunt:bush sunmr :uul
<br />lil:ll•.
<br />'I'hrsr sails :u'e poorly suitod W a'ildlil'o h:dlitat. 9'hry
<br />:ur Iypic:Jly used as habitat 1'ut' r:ul~rl:uul tvihllil'c, such
<br />:I: sr:drd quail :uul anlrlupc. I•ivrslurk ttrnrin(; must he
<br />vl•ry r:nrl'ully ncula>•rd il' arildlifc is to s:uisfy mast nl' it.
<br />hahil:n rcquirrnu•lus.
<br />'I'hr main Iinlitaliuu for rnnsn•uctiun un thl• tich:unhl•r
<br />sell is sleep slopes. Iluca use of rapid poruu•nbilit}•, there
<br />i- a hazard of pullutiuu il' this sail is usoll fur srpti[• l:mk
<br />:Ibsurption I'irlds. '1'hr hiy;h rnnu•nt ul' cu:u'sc I'ral!'mcnts
<br />m:n• c;uhr prublrnls \cith oscaentinns, mainly 6rc:msu cut
<br />bauhs c; n'I• in. Fperial dosigns I'nr buildings and roads are
<br />noorss:u•p to ~ll'srl the limitation ul' slope. Tlu~ Nazar soil
<br />i; limitol' by drpllt ul shnlu, slaty prrnur:lbility, limited
<br />:,hilily lu support :, load, shrink-s\ccll potcutial, lend slope.
<br />Muth soils :n•o limited by l'rnst•action pulonti:d. Special
<br />declass fur 6uib ling;s :uul roads :u•r nl~lyd to nvurcomr
<br />t hesc limitations. CopaLility subclass ~'llo.
<br />S:I-51:pda•lon s:mdy loam.:! to 5 percent slopes. 9'his
<br />deep, nonc~lla•:u'rous, a'cll draiucd soil located in sandy al-
<br />lut'ium derived from :u•I:osie herh•uck mt upl:uuls. T;Icva-
<br />liun r:utg:vs from 1y31111 to i,:IUU 1'cet. 'fhv avrr;l~c Ilmtuo,l
<br />procipitatiun ix :Iboul 18 inchos, the :n•rrag;a :nuw:d :,ir
<br />tong n•r:LLUrc is about •IT de{; errs I•', :uul the :n•crul;e lYust-
<br />1'rre paa•ial is about la:i days.
<br />Typic:d:y, the surface layer is }grayish brown sandy
<br />lualn about I! inchos thick. •fhc subsui{ is grayish brott'n
<br />~ravrlly sturdy loam about G inchos thick. Thu substratum
<br />r~l rods to a depth uC fin inchrs nr more. It is pule hro\c^
<br />p r~ crlly :Tandy lu:nu in the uppl•r p~u't ;nvl Kratios lu
<br />I~ravrlly lu:nnt• s:uul in rho la\rrr p:u•t.
<br />lurludrd tcith this soil in nulppin); :ur small wens nl'
<br />Luucicrs I:ilty cl:n• to:un, : to l.~ percent sluprs: Illakel:uul
<br />lu:uny n:uul, ] UI !1 percent slopes; ttoluntl,ine gravelly
<br />s:mdy loan,, n to :1 percent slopes; and Pluvaquentic
<br />IL•gdaquulls, nearly level. Also included :ur areas tvhm'e
<br />:n•I:use beds of s:uulstone :uul shale lu•e at a depth of (1 to
<br />da inchrs. Int•ludrd :u•eas make up about YU percent of the
<br />ulapgled acrrag; c.
<br />Ih•ruu•:Ihility ul' this St;q dcton sail is r:q lie 1. I'. ffectivc
<br />r•n~u np d~•pll, i. I;u inrhr. ..r nlnr, •. ,\c:Iihl Llr teal rr
<br />~'.q,.lrll )' i. nlu,ha:Il1•. ~In'larr ru nu l'I' i. ann. :uul lhr
<br />I ..'/.:I,',Is ut r,'u>U q, :VIII nlgl I,IuN Ill1l :1 I'c Illrn lrl :Il r.
<br />'I'bis soil is a-rd as r:I ng~ol:InJ, fur to ilJlil" Iclhil at, and
<br />:IS hun,esitrs.
<br />X;divr• •rrpl•t;nine is mainly !resters trhr:lt~rass, sidr-
<br />uals ¢r:uu:I. uoedloandthrr:ul. :uul liltlr hhlrs[rnl. '1'hr
<br />p rrdumiunnl shrug! uu this soil is u•uc mnuntainnmhu~:uty.
<br />1'urra occurs in .mac :u'cas.
<br />I h•1'rrrl•II t~raringt I:ur in :amtmor :uvl in I:,ll improves
<br />Ilu• ruudil inn of rho ran}o. 1'ropcrly lurating; livcstua•Ic
<br />o al el'I ilk I~dl'lhllen hrllr~ Lu t'u„!1'UI (; 1'a211,y;.
<br />1\'ind brr;lks :uul lat\'irnnnuart:d plantings :u'r g;cnerally
<br />snitoJ to this soil. Soil hloarin~ is rho prinrip:d limit alien
<br />
<br />iur tbc• rsl:d disluuo nt of trcr~ :Intl shrl,hs. '1'hi> llnlil:n
<br />c:ul ho nvrr[•atnr Iw cultivalinp Ilnly in Ihr U'rl' erns a
<br />Ir;l t'1lit: .I nll'ip of t'r}!rl:d iuu Lrl as ern Ihr 1'nta ... tiulgl
<br />n u'ntal irril:atinn may bo nrrd.•11 tchru phnuinp and .I
<br />in);~ dr.1' pcl•iw ls. 'l'eers that :ur ho>t suilrll :uIIJ have pI
<br />sureical :u•e Kncky Aluuntain •luniprr, rasu~rn rl ~rlrrd
<br />pnndrlv,sn pine, tiibrri:ln elnl, I: u.;ni:urnlicr, :old Icu•L h,
<br />r}•. Slu'ubs Utat :u•e 6rnt snitell arc shuul,l •u>.I, ..Inn
<br />lilac, and Siberi:,n peach rah.
<br />'I'bis sell Is salter! to hahit:u fnr opruland :Intl raup•'la
<br />trihllil'o. I::ut~rhunl \ciIJlilb. snI'h :I~. prnul;huril :IUII'II,i
<br />ran be encour:lt;ed by dovrlupin~ lirt•sUlc6 nalrril lt! I'ar
<br />tics, pruput•ly mnnal;iuti5 Iivrst ul'I. ~r:viup, ;InJ rrsrrJi
<br />r:uly;c anc~rr needed.
<br />'t'he main limitation ul' ibis soil I.w ,urban usI• is I'ro
<br />action poU•n till. tipecial dr.. i>_'n nl' roads :uul .accts
<br />nccessar>' to minimirr frost hoaco d;uuaµ•. Rprri:d pr:
<br />tires trust be prnvirled to minimirl• \cutrr cru.;iun ,nut s
<br />blu\vin); on cons[tvt•tiun siu•s \chore crg;r Lltiun has ho
<br />rentaved. Access roads mu..;t Gave adry u:nr cut-slu.
<br />g:rarle and bu provided \vith drains to cunu~ul surlLro t
<br />huff. Capability subclass R'u.
<br />7:1-Slttplelon sanaly Ioanl, ~ to Li percent slop!
<br />This deep, nnncalcarcou s, sell Ihainrd suit I~I n•nu•rl
<br />sandy :dluvium derive!! from :u'kusic hodrock nn npl:uu
<br />I:Irvation t•uuges from fi,GUa lu I::UU Coot. 'I'hv acrr:I
<br />:mnmll preripitatimt is about 1:. inchrs, thv avI•ra ~e :I
<br />nual sir twnpetmtw•e i. ahuut ~I7 dr); roc.. 1', amt t
<br />a veral;c frost-free period is ahuut l:;:i days.
<br />Typically, the sw•f:¢•o layer is grayish hroavn >:Im
<br />loam about 11 inchrs thic•Ic. `fhr subsoil is g; ra ~~ish brut
<br />g;r:wclly s:uuly loam nbuut G inches thick. '1'hr soh-u':au
<br />r stmuls to a depth M' [;u inchrs or nun'r, It is p:Jr brut
<br />Rru velly sandy guar! in lhr ulyu•r Iru•t luul pr;II II~s
<br />g,rarclly lo:lmy s:uvl iu the lutcor p:u•t.
<br />Included with this soil in waggling; :ur• sncdl :u•oas
<br />ft resser sandy loam, a to U pr rcont slnprs; Luuciorn sit
<br />clay lu:nn, 3 to IK percent slupus; 'I'rucklun s:mrly In:uu,
<br />to !1 percent slopes; 1'uder grracrllr s:uuly lo:un. 1 •tr.
<br />pmrcm slopes; and stall outcrop. of :u'kuso hell: of ..+:m
<br />stone and shale.
<br />Permeability of this Staplclun soil is r:q,i.l. 1:1'ircti
<br />rooting; depth is lie inchrs or stare. :1 v;ulahlc tc:u
<br />capacit}' is mudrratr. Jurlacr tonal! is ulrllnun, amt l
<br />ha z: u'•I of .•rusiuu i. laude rnll•
<br />'I'lu• sell is acrd :rv r:u lpr, I~•r o.ILIhII 1,;J•n.rt, .,nJ
<br />I IUII Il•?Itl'%.
<br />I~:dirr veg~rl;u ion is nlainl~' acoa,'ru t, 11. :npr.~~.. .III
<br />unls ylr:un:l. nredlr:nuliln•rad. and lilll•• I~Iw'-l••nl 'I'
<br />domiu:utt slu•uh un lliis ..ail i. trw• nwunl:IUUn.lhurar
<br />Yucca is presrttl in sumo Ilhu'os.
<br />6efola•ed firazing; late in sunuuor and e;u~l t~ ul f.Jl u
<br />proves the condition ul' the r:m~I•. I'ruprrlt I„+':uil
<br />IivrsUu•k u':It eriuh facilit its helps tII cool rl.I Fr:I:.ulp
<br />11'indla•caks anti rnciruuulrm:11 pl:ou ntps pou. v.Ill~ a
<br />xuilad In thin suit. tioil 6lnaculp Ir ,he nl,un liwil :u l,nl I
<br />the establishment of arcs :old slu~uL.. 'I'bis limitation c.
<br />he ocorconu• by rultivntiug uulr in th.• u~ee c. nts a~,
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