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<br />_ ~. <br />_' - ~,f -. <br />._ <br />'.t 'cF <br />.~ <br />:v •t.` <br /> <br />URAcc4,M.r_9c[ cr,,,p~y ZS -cS°% <br />. _~ -~' ._ <br />r <br />i ±'h<~sv strap to++:gr,y stoop soils am un strap fens, and val.loy amt m untain <br />si•tesl~r}~~s ut ele+mti~~ne of GSOrI to POr}n Poet. The a~•oreme annual prncinitation <br />la shoo'. 2n inohes, the m^an annunJ nlr t^mpr,raturv is sbr~ut 44°F., and tho aver•sw <br />fry+st-true noriod is-a'+nut H5 -to}•s. Tho 7,tllman soil oceupios the broe•}, slifhtly <br />coneavF parts oC the ,landsoape. It makes up ah„~t r+~ percent of tl:a +init. The <br />rr <br />unnamed eol+l,ly loam soil oaoupies the eor.owhst oonvoz positions. It makes up <br />about 45 poroont of the unit. 2111man -lii'fers in having a finer textured subsoil. <br />The Zillman soil is morie;atoly doep and woll drainod. It formed in Rlacisl <br />outwasfi from mixorl minerolofy parent materials. <br />T; pically the surfaco layer is rla-k }•••own str~ny loam about 3 inches thick. <br />T1io suL::uil is dark brown stony sandy olay loam shout 12 inohos thick. Tho <br />F= ~:'; . 13ubstru'.rm is vary stony loamy sand. <br />Ponn~,ahility le rapid. 1+'factive rnotinr. dopt:h ie 15 to 25 'Hobos and the <br />avails'+1~~ Mater cap•~r.ity is `.14 to O.1R in.~in. Surface runoff is s?ow ar~d <br />the eros.inri hazard is alifht. <br />The unnsmod cobbly loam soil fs modorat^].,y deon and well drained. It <br />Po^mod in P,lacia). outwasfi Eton nixed rginorolorrr nar~n`. matorials. <br />Tyrim,lly the aurfac, layer is dark brown cohhl~• loom about H }.ncios thick. <br />The subsurface is brown very cobbly sanl;• loam shoo`. 32 inohos thiok, This <br />Prades into Band, cobble, anti fre.vel ut depths between 4o and t.0 inches. <br />Pnrr+mability is rapid. RPfoctivH ,•eotin~~ depth ie 15 to 20 ino}:es anal the <br />avails+.l~r:at^r oap city is 0.06 to 0.11 in.~in. Surfaoe runoff is slow anal the <br />orosio•~ hncard is eliPht. <br />,F • -~ ~.1 <br />