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.:= ss.~ <br />R~~ <br />+~~~ -14rrmm±7 Col,hl~• L~.~am, 6 to 12 pArcont slopes <br />T <br />1 .., <br />' T1,is is s ~riwrdb+-#~ ~ioop, vmll d~•nin~+d soil on alluvial inns and volley <br />eideslorns nt ole~ati,,ns of 500 to 70n0 feot. It formed in sandstone and <br />al:ale a]lu~ium from Permian Rodl,od forma*.i~~ns. The avnraPe' annual precipitation <br />is about 14 incl~os, mean annunl air tomporature is about 46oF., and the avorape <br />frost-froo ported is about 10.'1 days. <br />j .. IncL,ded in this unit aro s,mll ar:;r.s of 32 soil, all having sL:poe of <br />, <br />to 25 norcent. <br />Tyl,•ically the .surface layer is reddish-;,rows cobbly loam about 18 inches <br />'¢, . <br />~ thick. The subsurface ie r•,d cobl,ly sandy loam about 17 inohes thick. The <br />,,..substratum is very oobbly or flagry sandy loam that extends below 60 inches. <br />1.... <br />"mount of cobble and flarstono increases with depth. <br />i y )~ ~ 1 <br />Permeabil.ty is rapid. .~'fective root?nP depth is 20 to 30 inohes. <br />~,~. <br />7•he <br />Available water onpacity is 0.10 to 0.14 in.~in. Organio matter content in the - <br />. _ i ~.. <br />surfacb.2eyor is Sow. Surface runoff is slight and erosion hazard is,moderate. <br />This soil la used for hayland in some areas. However, tho~prinoipal use <br />is as ra~ROland due to stoninees and low waterholdinR capacity. <br /> <br />Iand Capability Dniti 6S (irrigated) <br />6S (non-irrigated) <br />Range'Sito~ Stony Loam <br />~r <br />.'. <br />