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TABLE I-1
<br />SOILS IN THE STUDY AREA
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<br />PICEANCE SITE
<br />Rlo Blanco Counly
<br />6 Uarcus channery loamy sand Barcus Alluvial (ans and nartow 2-8 Channery loamy sanJ, chennery sand Deep 180 4
<br /> valleys
<br />40 Ilagga loam llagga Flood plains anJ alluvial valley 0-S Loam, silty clay loam to loamy tint Dccp 31 <l
<br /> floors sand
<br />41 I lavre loam Ilavre Flood plains anJ low stream 0-4 Loam, fine sandy loam to clay loam Uecp 7 <I
<br /> lerfatl`5
<br />70 Redcreek-Rcnlsee complex ReJcreek Mountainsides anJ ridges 5-30 Sandy loam, channery sandy loam Shallow
<br /> Rentsac Mountainsides and ridges 5-30 Channery loam, very channery loam, Shallow 29 <I
<br /> sandy loarn and very Raggy loam
<br />73 Rentsac channery loam Rentsac RiJges, foothills, and site 5-SO Channery loam, very channery loam, Shallow 2,303 56
<br /> slopes sandy loam and very Baggy loam
<br />91 'forrionhcnls-Rock outcrop -- Extremely rorigh and eruJed I5-90 Torrionhenis are highly variable bur a Very shallow
<br /> complex areas on mountains, hills, typical one is channery loam, very to moderately
<br /> ridges, anJ canyonsides channery loam, or tint sandy loam. deep
<br /> Rock nulcrop consists of barren 838 21
<br /> escarpments, ridge caps, and points of
<br /> sandstone, shale, limestone, or siltstonc
<br />104 Yamac loam Yamac Rolling uplands, lermces and 2-IS Loam, clay loam, silt loam Deep 696 17
<br /> fans
<br />P1PELtNE
<br />Rlo Blanco County
<br />6 6arcus chennery loamy send Barcus Alluvial fans and narrow 2-8 Channery loamy sand, channery sand, Deep 187 9
<br /> valleys
<br />IS (:astnerchannery loam Castner Mountainsides, ridgetops, end 5-SO Channery loam, cobbly loam, very Shallow 104 S
<br /> uplands chennery sandy loam, very Baggy loam
<br />33 Forelle loam Forelle Terraces and uplands 3.8 Loam, clay loam Deep 5 <I
<br />3 Glendive fine sandy loam Glendive Along drainageways and 2-4 Fine sandy loam, loamy fine sand to sill Deep 315 I S
<br /> alluvlel valley Boors loam
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<br />z~sruum.iaoc mivsrpurMyarrn Sheet I of 5
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