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JUL-26-1999 14 01 SRN MIGUEL 13RSIN SCD <br />r.uni[unnt~wL wtu uwunrrirun~unr <br />Int. Uranluu <br />Hap Snil nave and destnption <br />Synbol ; <br />The poloagpe soil is deep and well drained on fppL <br />slopes :nd alluvial fans. It forned iri alluviun and <br />cdllunum from sandstbne. ivpually, the surface iaver <br />is extrenelY stony loan 4 inches thick. Tne subsurface <br />laver is loan 11 inches thick. fhe upper 30 incnes df <br />the underlying natenal is tine sandy ioam. Ine Ipwer <br />; Dar[ to a depth of o0 inches is loan. Rerneability is <br />; wotlera[e and the available water Capacity a logo. <br />Surface runoff is nediun to very rapid and the hazard <br />nt water erosion is noperate to very hign. the <br />effective roohnp deD[h is a0 or pore lncnes. <br />the Chilton Soil is deep and well drained on foot <br />slopes and alluvial fans. 1t forned to alluviun and <br />cplluvlun trop sandstone. lyptcally, [he surface laver <br />is stony floe 5ar~dy la an o inches thick, the <br />nntlerlytny material to a depth of oG inches is very <br />gravelly hoe sandy loan. Perneabtltty is ndderately <br />raped and the avatlable water capacity is lpn. Surface <br />runp}f 15 metli un to eery rabid aid [he na:ard of water <br />erosion is node rate to very n1yA. The effective <br />roohnp depth is 6tl dr nore Inches. <br />Land Capa btli [y Untt hlRk 6e. <br />81 Aock Uu[crpp <br />; Rdtk p0(L'rpp Cpn5i5 C5 pt la rqe exUd5tl1e5 Or detlrCtk <br />; Land ;apabillty Unt[ H1AA 8s. <br />ae , Hock Uu[crbp-Urthents uonptex, QU to 9q oercen[ slopes <br />Ihts roan umt 15 SU oercen! AOCk pp[Crdp and 3i percent <br />Or[nen[s 5011. <br />Aor.k outcrop consists of large exposures of bedrar.k. <br />• <br />970 327 4245 P.04 <br />Received <br />J!!( 2 71999 <br />Du~~ F'g <br />Gvision of fli~erafb8 GeplogY <br />