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• BOULDE~hJbit±RBB~LORADO • Rte? [o fA inches. reddish~bmtm f?aTR 5/+1 nnnralcare- mt; Lyons samLa.one n-it3 8agsione clearege. The AI horizon ranges from U to + inches in thlctnes=. and the A? hnrivm ranges from i to 1S Inrbes in thickness 'The A horiu~n ranges from loamy doe sand to hoary Ircamy ynd in lrvure. The B?t horizon ranges from 14 [o ?+ inches in th lcklle3e and from heavy clan loam to clay In texture. Amooat of ;tons ranges from &7 [e h0 herceot [hronghon[ the proale- Pinata•Rock outcrop complex, a to 55 percent slopes IPrFI.-This complex is on upland ridges in the north- cyestcrn part of the Area. It is about 4.i petrent Pinata eery stony loamy fine sand and about 35 percent Rock outcrop. Thr Pinata soil is throughout the areA but main- ly- has the smoother slopes Hock outcrop is scattemd throughout the area. but mainly has the steeper slopes. Yapped a-ith this complex along drainages~ays are small areas of n Pinata-like soil that overlies sandstone at a depth of mom IhAll ~k0 inche=_. \rear ridgetops are .s-::r~.-. , ,,,,~- - -- :.~; 'L.S Mme soils that overlie sandstone at a depth of less than 40 inchr:. :1 fen- areas of ('olhn-ial land nre also in- cluded. These included soils and Colluvial land make up allout ?(1 pefunY of each mapped area. RunofT is medium to rapid on areas of this complex. The erosion harard is Iti~lt- Mort of the acrw~c of this complex is used for forestry and limited grazin_ of livestock. A major use in recent tears is for quarrying of hnildin_ stone (Capability unit CIIe-1. nonirrieated: trey suitabilitc group 6) Renohill Series The Renohill series is made np of mfxlerately deep, mcll-drained soils. These soil; formed on upland hills and rid_oes in lonnly parent material n-eathered from shale and sandstone. Slopes are 1 to 9 petcent. F.leyutions nm -4,9t1n to 5,0(1 feet. The native ~-e~aetation is mainly Figure 3.-Profile of Pinata very stony loamy fine sand in an area of Pinata-Rork oulcroD comDlez, 5 to 55 percent slopes.