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'°-h'!f`--1~•~,rt.-W~xn1.1 r,r.t,r~~m•,ly r.~l,hly :;•~n~iy lonrm:~ t.n hS I„•rr.r•nt. ::1on~•;•. <br />I 'fiie:u• ore challo;r rmd mod~;rrttely dr,ryr, well druinr~rl soil.n urn.lcrlnin by <br />};r:,nit,• hudruck. kogr~rt ;:oils nre~ uieillow null cnu,}u•i;,c ubottt ~0 1>crcunt <br />of the nrcu. Woodhull soils are mrxlerrttrly deep and comprise about 40 <br />percent of the nreu. kogert soils are on steep side slopee and ridges, and <br />Woodhull soils are on morn level side slopes. Included is dee}~, sourly <br />loom soi_1 on foot slopes and in narro•.~ drainngeways. Also included is <br />about 5 percent Rock outcrop on ridges. Ro er soils are mainly extremely <br />cobbly sandy loam with a thin layer of extremely gravelly sandy loon <br />above the bedrock, which is at less than 20 inches. The soil is slightly <br />acid to neutral. Permeability is moderately rapid, and available eater <br />capacity is very low. Typically Wood} soils have extremely cobbly <br />sandy loam surface, very cobbly clay loam subsoil over granite bedrock <br />at 20 to k0 inch. .depths. The soil is slightly acid. Permeability is <br />moderate, and available water capacity is low. Limiting features are <br />steep elopes, shallow and moderate depths to bedrock, and the high <br />content of cobbles. <br />NonirriUnted capability subclass: Vi Is <br />Range site: Shallow loam <br /> <br /> <br />