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<br />` ~tiV t.~V Ill 111 111111111!
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<br />dl
<br />u\iuut.
<br />ranulge-
<br />!u pastor/' :nut rcllivo ;;
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<br />u'rtgated: ~YcL Alend
<br />cv
<br />
<br />I`:}I•s. (':yrrbilil}' unit IVIC-1, 1
<br />999
<br />Cap;linnl.y unit i'Ir :.
<br />.h•
<br />
<br />Pt. Slopes u
<br />;Illllll)' g1'n^h Vii. rnuy;e site: evimdbre:tl, suit ,
<br />si 'not assigurrt Inn .c
<br />~ sedges. 1S6 Punu•r-liue6 cute
<br />t gl'm5SC5
<br />from l:; ~
<br />1 urner ti~rie, 1 1 elulll•N. 'I I11S Cllmples
<br /> .,r steep suite nn upland
<br />ges from
<br />The earner series consists of shallow. \vell drained percent I urner lute smnd
<br />ges from soils that fnrnted in material weathered from reddish fuck o~in1,~I:nllittPactkimlt
<br />Irrutvn sanrlstunP. 'I'hesc soils :u'r un upl:uuis :uul ;u'e less slo n
<br />is ;[ray underhlill Iw s:uulslone :11. :1 depth of IU 4. ~U inches. the o•estorn side of rid;tr:
<br />1 inches I?Ievaliun rnngos Il~om fi,Hf10 to G,~ 011 feel. Slopes :u'c Included with Illis loll
<br />e sumt\' 1 Gr aU pc•rcenL '1•he ualive vegeLtltio^ Is nntinly blue cent areas of I~irtlry .,ail:
<br />f:unofl' is rapid.:IUd th
<br />tvailable b't'ama, ~ehealgrassas• mount:tiumahogarty, and some This soil is suited to n
<br />alkaline. other im'bs and shrubs. D4ean annual precipitation ~'lle-1, dryland; Turner
<br />tzing..q r;mges from ] ; to lf, io ches, mean annual air rem rera_ site and Ruch outcrop no
<br />lure. tore ranges front ~17 to 43 F, and the frost-free assigned to ;t \+•indbrexk s
<br />~ loam, 0 season r:ut>,res fium I lF to ]:ill days,
<br />feet cost In a r'epr'esentative profile the surface laver is
<br />t. G9 ~4,.: reddish brnu'n fine s;lndy loam about i inches thii•k.
<br />to sandy The underlying material is light reddish brvn'n tine
<br />moist; saluly loam about 7 inches thick. );elon• this is hard
<br />tructure; reddish bro\vn sandstone.
<br />cky and Permeabilih' is moderate, and the available water
<br />ce tech eupatcity is low. Reaction is mildly' alkaline above a
<br />um and depth of about 7 inches and moderately, alkaline below
<br />deratel\• that depth.
<br />These soils are used mainly for natice grasses.
<br />(10YR I,epresentati\'e prolile of ~Purner tine sundv loam. 1
<br />gt•ayislt to SI percent slopes. in nati\'e grass, about 1,0011 feet
<br />rnon me_ north and G50 feet evert of the south\e'est corner of sec.
<br />brotcn `?O, T. 70 N., I.. r0 lV.:
<br />s; weak Al-Il to 7 inches; reddish bro\v^ (5YR AB)
<br />tructure fine sandy, loam. dark reddish bro\vn
<br />,teed soil (i1~R 3/3) moist; weak tnedittrn cub-
<br />e: many :mgular and weak to moderate medium
<br />uu'emts; granular structure: slightly hard, cet;v
<br />smooth friable: c:dc:u'elnts; mildly alkaline; clear
<br />smooth bound;u•y,
<br />(lOYR Cca-r to ]'1 inches; light reddish brou'^ (5YR
<br />brown fi/3} fine sandy loam. reddish brown
<br />promi_ (51'R 5/8) moist; weak medium sub-
<br />R G/4) angular blocky structm'e; slightly hard,
<br />v buret, very friable; calcareous; visible second-
<br />tplastic; aty calcium cu•bumtte as seams and
<br />ry •utd streaks and finely divided forms; moder-
<br />tlakes; g-19 to 60 i iehes;lha rd reddish\brolwnrs•<tndstone,
<br />o sandy The A horizon is sandy loam or fine sandy loam 6 to
<br />mottle 1' inches thick. Content of rock fl•agments, mainly
<br />tgmeuts gl';tvel-size sandstone, ranges from Il to 15 percent.
<br />es from The A horizon is leached of lime for a few inches in
<br />is ;tt ;i Maces. The zone of lime acenmulutintr is itmnediately
<br />cleave nr in the upper p;u't of the hrdrock in places.
<br />Hlupre, H.>-I'u race line handy lua m. I In 9 peree•nl nlopen.
<br />'Phis m'ar'Iv Ir•vcl U+ str'omgl}' ,loping soil is ou upl:uuls
<br />a' small :Ind ridges. 'I'bis sail h;IS Lhe prolile described as
<br />>d :ere a representative of the series.
<br />of less Ltcluded with this soil in mapping are some small
<br />r small areas of soils that have ;t surface layer of loam. Also
<br />included are small areas of soils that have more stones
<br />;ht. in the surface layer, small areas of Lock outcrop, and a
<br />tl hay. fe\t• .mall ;u'eas of Kirtley soils.
<br />ox'rt if P~rto]f i.c rapid, and the haz:u'd of et•osion is severe.
<br />suited This soil is suited to pasture and native grasses.
<br />LAI:IMI;Ii 1'In iN'
<br />I:rnll; tihall~,s Ih ndhill r;m>;
<br />ndbreak sulLlbililc >;runl~.
<br />up cungdr~, 111 dl Sfl pet
<br />c,nlsists of nurclcratelp sloe
<br />and rid);cs. II Is :Ibnut ••"i
<br />In:un :Ind about ;SII pcrccn
<br />s:uuly loam iv snwother art
<br />crap is steeper commonly' u
<br />iu ntnpl~inc is about I..-r prl
<br />hazard ul' rra~ion i. seccrr.
<br />live grasses. Capability uni
<br />oil in Shallow Foothill rang
<br />assi},•ned to a range site; nu
<br />iitahility' group.
<br />lintni:c Seric~
<br />The P,at:Ike series co
<br />cn• somecehat excessivel
<br />material weathered fen
<br />'these soils •u'e nn upl:
<br />;end u'e underlain by
<br />.eeathered granite ut a 1
<br />lion ranges from G.SOu
<br />fro percent. The native c.
<br />side-oats gr:una, strudel
<br />grass, muunLlinnulhug~
<br />precipifalion range, feu
<br />;tie temperature ranges
<br />frost-f rce season r;ulges
<br />In •e represenlativr
<br />reddish ~~rne• chanucr;v
<br />'fhe subsoil is reddish bl
<br />:r inches thick. The unI
<br />phyllite ur phyllite schi;
<br />I'et'meuhililp is noel
<br />capacity is low. Reactio
<br />These soil. are maim
<br />Represenlatice prufi!
<br />an area of Rnlnke-Rae
<br />cent slopes, in natice
<br />the southwest corner of
<br />.91-0 to 10 inrl
<br />cllannery-
<br />crumb st
<br />percent s
<br />mire cui
<br />Du u n d:u•y
<br />R4-IU to 1''i inrl
<br />e'CI'P t'lt,
<br />(:,Y I: 1
<br />:wguLu'
<br />strung li
<br />flu perce
<br />mica cot
<br />GI'-I i to °:, I
<br />phyllitic
<br />eve:dhcr
<br />hand w i
<br />signitic•;1
<br />of the sl
<br />sits oC shnllmc, well draine
<br />drained soils [hat formed ii
<br />\ granite, schist, or phyllite
<br />ut ridges and mount;tinside
<br />Feathered phyllite, schist, o
<br />eptb of 10 to 20 inches. Cleva
<br />G. ii,:iflir feet. Slopes are 1 t
<br />gcl;tlion is mainly blue gram:
<br />whcutgrass, bluebunch wheat
<br />ny, :unl sage. D(can nnnua
<br />i I'I tm 18 inches, mean nnnu;i
<br />llvm 1_t° to 4(i° F, and th
<br />f ram 75 to 11N1 days.
<br />profile Ule surface lat'Pr i
<br />h,:un about 10 inches thicl
<br />rwu ver}' ch:uuterv la:un abuu
<br />~rlving material is \cealhere
<br />rate. and the available \cnte
<br />t is ncuh;tl.
<br />used for native grasses.
<br />of Ratxke ch;utnet;v loam i
<br />outcrop complex, ':\ to G5 pert
<br />rays, about °.:;50 feet east 1'I
<br />sec. Vii, T. S N.. R. 70 ~1'.:
<br />us; reddish gene (5YR 5/'2
<br />In;un, dark reddish hru\vn (51
<br />;t; strong line granular arV
<br />vcturc; so1•t, vet.v friable; 7
<br />ft phyllite channels; vet;v big
<br />lent; ueu[ral; clear smuol
<br />rs: retldlsh brown (~iYR ~i/:
<br />unery loam, reddish brn\t
<br />:.1 ntnist; nxnier.lte fine su
<br />hl,rln~ s(rurtu re pa cling
<br />Ie ,r:umd:u'; salt. vcrc 17iabl
<br />t phyllite charmers; very, hit
<br />eat; neutr;ll; dilfuse lrnund:u
<br />Iches; u•crthcrcd phyllite
<br />schist; co:u•sc fragments a
<br />1 :rnd c•an be crushed in t
<br />h some dilliculh' but n'itho
<br />t contributions to the fine pat
<br />I on lust anct second breakage
<br />
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