Laserfiche WebLink
'~~28F ?il lr~an-I)nnamod oobbly loam. sY.eop to vory s• p <br />:~ <br />Tli~se stoop to rvery steep soils aro r+n atoep lane, and valley and m~ rintsia <br />i i} <br />diAY. <br />`~ . <br />~: ~ <br />ir:. <br />;:. <br /> <br />~: . <br />.sideslopes at elevations of GSOrI to R000 feet. The e~ora~e annual preoipitation <br />~is abou'. 2~ inohes, tho mean annual air tnm~erature is about 44°F., and the average <br />fri+et~Proe npriod is a[+out 85 ~inye. The 7.illmatt soil oooupiea the broad, slightly <br />oononvn, harts of the landsoape. It makes up ab~~ut ,5 peroent of the unit. The <br />unnameA oohhly.loam soi]; oooupies the soinowhat oonvex positions. It'makes ~tp , <br />I <br />about 46 peroont of the unit. Zillman differs in having a finer textured subsoil. <br />.The Zillman.soi'1 is moderatoly deep and wall drainod. It formed in glacial <br />outwash from mined mineralogy parent sgtorials. ~._ <br />T+•picnlly the surface layer is dark b~•own stony loom about 3 iriohee think: <br />Tho s,rbnoil is dark brown et •uy sanr~jr oley loam about 12 inohes thlok. The" ~. <br />avaita~+ln water cepcoity Se 0.06 to Orll in.~in. Surfaoe runoff ie stow and ,the <br />,: ; t, <br />r~,,,;{,;:subatrntum is vory stony loanp. sand. <br />' Pennrab111ty Sa rapid. uffeotive rooting depth is 16 to 25 inohes grid ;ties. <br />availel+ln water oap~oity is ~+.14 to.0.1R in.~ih. Surtaoe runoff is slow and;. <br />. ~ <br />the erosion hasard ie eli~ht. <br />The unnamod oobbly loam soil is moderate)y deep and. well drained. It ~. ' <br />Po^med fn Placiel outwash from mixed minerolo~ parent materiels. <br />Tyrionlly. the eurfaoq layer is dark brown oobbly loam about 8; inohbs'.tFfiak:.' , <br />The.atibsurfnoe is brown very oobbly sand;r loam.abou*.'82 inohes thiolk. This', <br />gnsdee into sand, nobble, and gravel at depths between 40 and [i0 inohes. :•:~' ' <br />Pes'•meability is rapid. SCfeotivs rooting 3epth is 16 to 20 inohos ea~:~he <br />:'~;~~. <br />":a <br /> <br />erosi,or~ ha card is slight. <br />~%. <br /> <br /> <br />