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<br />VR=Vorsid-Rock autcrap complex, 3 to 10 percent slopes <br />~andforrns: Undu!a.ting ridges <br />Cgmposition <br />Vorsid sr~ll and similar L•~clusions; 70 ~rer[ent <br />Ruck autcrop: ;5 percent <br />Contrasting inc!usii~ns: 15 percent <br />Cfiaracteristics of the Vorsid Sait <br />Fart n( Iandfarm: Intermingled vlth, Ro[:. out[rop <br />Slope range: 3 to i0 percent <br />Parent msteriaL• find=residuum; s:~:r[e=grarwd~or~te <br />Native plan, camma:nity type: Grass <br />typical profit?: <br />0 tri 3 Inches=dart; Grouu gravelly sandy loam <br />to 3 inches=Brmun gravely sandy loam <br />3 inches=granedion to <br />Depth ctas>: Very st~a!lov, shallow <br />Drainage class: 'Ae'' or snmevnat excessively <br />Permcabiiity: Mi~derate ar~r, mnderateiy rapid <br />Available stater capac,ty: Very loo <br />Potential rooting depth: 4 to ~0 Ir.[hes <br />Runaff: 5lnu to rap,d <br />• Hazard of Wafer erasion inn plant cover!: Sight t,, high <br />CF~aracteristics c.f Rock autcrap <br />Part a( landferm: !r,terming!ed vith the Vorsid soil <br />Xind of rock: Srar~odierite <br />Form of outcrops. Starry and Bouldery outuaps to 5 feet high; areas of er.posed Ged-ock surface aSout <br />1 to :~ fee: ir. diameter <br />Contrasting ?nclusiorrs <br />Ir. con[ave drainagevays betueer~ ridges; deep and very deep si~ils with thick, dart: surface layer <br />inter:Ain~led 'dith t`:e s2 ~/pr51d sA:IS; SUi!5 Ilnderl a~ri at S~:a'. 6W dep th5 `.~)' Ve at`.er2d BedrOCk <br />Similar Inclusions <br />Intermingled uit.`i the Vorsid soil; s`:allou sn:is that average siigtaly ;ni~re aan 40 percent crava! ,y <br />volume <br />Major Uses <br />range I ar,d <br />Major Management Factors <br />Soil-related (actors; Shal kw depths to Bedrock, very !ov available voter ca achy, [ommon outcrops u+ <br />Gedra[k <br />Climatic factors: <br />Mean annual precipltatien=l0 to 1~ inches <br />Me:r~ ar~r~ual air temperature=35 to 40 degrees F <br />Frost-free period=50 to 30 days <br />Elevation=3,500 t[. 3,700 feet <br />Management Considerations <br />