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7UL-26-1999 14 00 SRN MIGUEL BASIN SCD <br />' dONTECNN1Cpl SUlLS UL5U H1vIlUn ~UNi <br />lnt. Uranlurt <br />Mao Soil nave and desc rl ption <br />Synbol ; <br />45 Gladel-eond-Hock Ou[croD coaplex, i to 50 percent slopes <br />ihls nap unit is 3! Dercent Gladel soli. 30 percent <br />Bond soil. and 30 percent Adck putcroD~ <br />the Gladel soil is shallow and well drained on news. <br />bencpes. and eSCa rDmen LS. It forned in re5laDUm 1lpw <br />sandstone. frptcally, the surface laver is sandy loam <br />; 4 inches thick. Tne underlying nalmrial tp a depth of <br />; G Cnches is santlr loan. Perneabiltty Cs nmoerately <br />rapid and the available water capacity is very low. <br />Surface runoff is slow to very rapid and the narard pf <br />; water erosion t5 slight [o very hipl~. the effective <br />roaring depth is 8 [u 10 inches. <br />The Hond sot] Cs shallow and well drained pn mesas, <br />menthes. antl ascarpnents. It forned to resrduum frdn <br />sandstone. TYptcally. [he Surface layer is hne sandy <br />loan 1 Cnches thick. the subsoil to a depth of 16 <br />inches is sandy clay loan. PerneabiJlty is noderate <br />; and the available water capacity is very low. Surlace <br />; runoff IS 510M tp very rapid and [he hazard pf water <br />; eronpn 15 slight td uerY high. the effective radtind <br />depth 15 10 to 10 inches. <br />Hock outcrop consists of garde exposures of bedrock. <br />rand ~apabtlity Unit N1HA 7e. <br />Land C7 Dabtlity UnIC NIHN 85. <br />79 ; Poloaque-Chilton conplex. 5 to 3U percent slopes. <br />extrmneiv stony <br />This nap unit is SU Dercent Po luapue soil and ]: <br />percent Chlltpn soil. <br />• <br />970 327 4245 P.O3 <br />Received <br />JUG 2 q lvg9 <br />~~rd <br />DMapn a/~ e f ~ $ Gep °i9Y <br />