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~-, h • <br />/ III I II I II I II IIII III r~ n -) <br />~~ ~ ~ ~~ <br />53--Pinon-Pcwdi El:-Frock outcrop cot. ~l ex, 3 to 3P ;crc^_nt rlc,•as. <br />T`.:i~. :,.^p unit is e^. !^er:as, b~=nr.hc•s, zn? c~sc_trn°ccts. T~~e n..'}•;c veeF:c[i~,^ <br />is ~;r.n1y ni•.vnn lane sad _t,h ._;,er. F]?. ._.~; r. i~ ~,3';'• Co .°r'' [Hr- <br /> <br />~.- ^7 _ _ .' Lr' .i ., - ... -_.+C rte.. ... i• <br />~: L15 C31t ._ ~J net CenC !'ii`f•^. 70a::, 77 P°:'re^C 1JV~'Sli l0"..^:, of ~ _- pP!_ <br />C~_aC 6a: t: ,n~L Pr„p, lae fem. O'dd 1S', :!131 n^_';rs .iiC^_ i~:' i3,;C 1•ru= ~ n.._ .~.,_ <br />u:~~'_e-sCOry are thicl:e:. Ruck uuterc,p a,;:':~, u;. ..., r.:uc'~ as 35 to wU p~-cenC <br />of sc~~~? mapped .,teas. The Rocl; outcrop orccr= throuchoui the map unit as <br />lu;:: _, 'CS C`n esca: pn~ents Or a5 qJr Cr JpS :.a the .`latte7 S1Gne5. <br />Inc'.i.ded in this unit is about 5 p>rcen[ Progresso soils occu:ring <br />under more open };rass-shrub areas, 5 percent sci7s that are similar [o <br />C.t.ese Pinon and Bowdish soils but have greater than 35 percent rock fn~(:- <br />:rents in the control section, 5 percent soils that are similar to these <br />Pinon and Bowdish soils but lack a calcic horizon, and 5 percent variable <br />Ustic Torriorthents occurring in areas with thicker understory. Ai so <br />included are small areas of Clovis soils and tieville soils occurring on <br />alluvial fans. <br />The Pinon soil Ss shallow and well drained. It formed in residuum <br />derived dominantly from sandstone and shale. Slope is 3 to 3G percent. <br />Typically, the surf~3ce layer is brawn loam about 5 inches thick. The <br />underlying ¢aterial to a depth of 16 inches is pinkish white loam. Hard <br />sandstone is at a depth of 16 inches. In some areas the surface layer is <br />gravelly loam, gravelly sandy loam, sandy loam, or cobbly loam. <br />