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PUILLIPS COUNTY, COLORADO <br />! • f t i <br />t ? r <br />t ' <br />t <br /> <br />. ?l \ • <br />. 7 <br />h i(/urc T. Profile of `, alentine sand showing the thin surface layer <br />strucinrt• that breaks to single ;;rain Istructuroles8l <br />1 t•ry ?„ft Wlu•n dry , eery friablt• ht h ose N\Ileu taoist ; <br />;tradual, smooth honudary. <br />t'-12 to 11 inches +. yule-hr„ten i IoYR J;31 fine sand. (lark <br />brown i I0YR b'31 when uu,tst: sinule krain istruc- <br />tureless) ; l,a,se Mien dry anal nwist; n„n,•al,•at•,•on:. <br />Tht• A horizon rangos, frmu 0 to tt hwhes in thickue.ss. Tlw <br />lhwkest .snrfac•e Myers are in the least sloping areas. <br />'I'll" Valentine soils Are ussori:,tril Willi the .Iul,shur? suits. <br />yalelltil,• s„ils h:M' a Thinner surface layer than the .lilt- <br />1 nil%; s its :i i i t I Ii,s tl:ty in the ulttlericin, layer. Valeatitle <br />-6, are it•ss \t"eil detleh,ped thrnnLh„ t[t the In„ file 11;1ta the <br />.tulesl,ur;; wits an l li:tct• le,s Ili, kuess ?f dark •-,it materint. <br />Valentine fine sand, rolling ;V,_-DI ovetipies most of the <br />andhills that are Southeast of Holyoke. This soil is asso- <br />iated witli Hamlin soils in some small areas in the north- <br />lmtral and northwestern part, of the county. Slopes :ire <br />Iltotlerate to steep. 'I'lte prolil, of this soil is similar to the. <br />"Ito ,lr,rrlbedas typical fortlie>cl'hs. <br />Included with this soil ill utappilig, were a few slimll <br />,Aowollt, t,', acre to 5 acres ill aIzt-. 'I lleje areas ell'e shown <br />„n tile, Soil slap by a symbol. <br /> <br />uils \"alentine Soil i extremely tlrtlllglity in (Irv }'ears, <br />plainly because it is excessively tfrained 111111 low 111 avarl- <br />able water holding capacity. This soil has very rapid <br />permeability. <br />Growing in most areas ire sandreed, Sand bluestenl, <br />switchgass, needle-and-threml, and other native mitt and <br />tall grasses. This soil is well suited to these plants, but <br />,•razing should be limited because of Susceptibility to <br />severe blowing. This soil can he reseeded w ith adapted spe- <br />cies of native gasses, but the steels slopes make manage- <br />ment difficult. A felt/ small areas ire cultivated, mainly <br />for the Rntrpose of squaring larger held, of other soifs <br />:slid nuking them easier to cultivate. Capability unit. Vle- <br />(dryl:ut(l) ; Deep Sand range site; windbreak suitability <br />gr•oIll, I. <br />Valentine tine sand, hilly (VaE) occupies dunelike areas <br />that Mace steep, alrupt slopes on the leeward side. This soil <br />is ill til stmt It cent rat and southeasteI'll parts of the coullt.y. <br />The surface layer of this soil is severely eroded, is very <br />dark :,,ravish brown, and is as rlmch as inches thick. <br />Till, soil is suited to native orrasses, but extreme limita- <br />tion, ;ire needed to prevent overgrazing. Eveli though the <br />plant cover generally is increasilig, many areas Wile nearly, <br />bare. Iievegetation is extremely ditfirult, though it ran be <br />done through careful mallahelllelit of grass 111 blowouts <br />and of annuals and yucca. This soil i, droughty because <br />it is very rapitllti• permeable, excessively drained, mA low <br />in available water holdir[g caliarity. Capability spilt V1 le- <br />i (dryland) ; Choppy- `and range site: windbreak suit- <br />al;ility group I. <br />Wages Series <br />The Wages series consists of Ile1p, well-drained, loanly <br />soils that are gently sloping to steep. These soils occllltY <br />the side. slopes of intermittent stre:uus (ti(". 3), and most, <br />areas are alonor Freurlinlan and Patent Creeks. Wm,vs soils <br />formed in a recldisll-brown nraveily deposit. Tlie upper <br />part of the soil has been mixed with some windblown silty <br />material. <br />In a typical profile the surface layer is gravish-brown <br />Loam about 5 inches thick. The Subsoil is about 11 inches <br />thick. [m the upper part it is Clark ;ravish-hrown, slightly <br />inird clay loalu that is about. 5 percent title gravel. The <br />lower part 1, stilly, l-ht brownish-gr'av clay loath that r5 <br />abollt o to 111 percelit Lille _ravel. <br />At :l depth of lfi to 21 inches is verv strollgly calcareolls, <br />li dit hrowilish-gray loam. Below this is light-brown <br />,ravt•lly,study Icmill that is free of lilliv. <br />Cages soils are moderately to slowly permeable :11141 are <br />well drained. Be,-allse they have a thin loam surface <br />laver over a slowly plrtlle:tble clay loam sullsoil :Ind are <br />gently sloping to steep, Surface runoff I., mctliuin to rapid. <br />Because their subsoil is somewhat rr;IVelly thtsY hive <br />moderate available Nvater holding capacity. Wages soils <br />are Moderate ill Ilatunil fertility. <br />A14 11i7' Intl slupl, Of Illt11•1hitt111t ArV:lllta aIV a. few <br />:1111:1, of 11-at:es Ft,il, that :tl'e -till in native s;ra,s, mlainly <br />wt. tivrll t%heatgrass and blue yl'ama. (iraSsvs ar•c ht-tter <br />suited than roiv crops, all([ only :i few arl•es are 41111tivated. <br />These. ,oils call be seeded to grass.