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Northern San Isabel amf Western Pike National Forests. Cok:ratlo <br />MAP UNIT SETTINGS <br />Location: alpine areas where igneous an <br />metamorphic rocks predominate. <br />Landform: cirque bottoms. <br />Parent material: glacial till, co!luvium, and <br />alluvium. <br />Geologic symbol: Qa. <br />Elevation range: 11,600 to 13,000 feet. <br />Aspect: all. <br />Climatic zone: alpine. <br />Mean annual precipitation: 30 to 50 inches. <br />Mean annual air temperature: 34°F. to 38°F. <br />Average annual snow/all: 300 to 500 inches. <br />COMPOSITION <br />35 percent Moran and similar soils. <br />30 percent Rock outcrop. <br />20 percent Cryaquolls and similar soils. <br />Contrasting inclusions <br />10 percent shallow soils with a dark surface on <br />ice scoured convex slopes. <br />5 percent soils that lack a dark surtace, near <br />timberline and on exposed convex slopes. <br />TYPICAL PROFILES: <br />Moran <br />Surface layer{s): <br />0 to 2 inches -dark grayish brown, gravelly <br />sandy loam. <br />2 to 10 inches -brown, gravelly sandy loam. <br />Subsoil layer(s): <br />10 to 20 inches -yellowish brown, very gravelly <br />sandy loam. <br />20 to 32 inches -light yellowish brown, very <br />cobbfy sandy loam. <br />Substratum layer(s): <br />32 to 60 inches -light olive bro.vn, very cobbfy <br />sandy loam. <br />Cryaquolls <br />Surface covering layer: <br />4 to 0 inches -dense mat of partly decomposed <br />vegetation. <br />Surface layer(s): <br />0 to 12 inches -black, sill !cam. <br />12 to 18 inches -black, very gravelly silt loam. <br />Substratum layer(s): <br />18 to 60 inches -dark greenish gray, very <br />gravelly sandy loam. <br />SOIL PROPERTIES AND QUALITIES <br />Moran <br />Effective rooting depth: greaser than 20 inches. <br />Drainage class: somewhat excessively. <br />Depth to seasonal high water table: greater <br />than 6 feet. <br />Available water caoacity: low. <br />PermeabUlty: moderately rapid. <br />Runoff: medium. <br />Rock outcrop <br />Landform: ice scoured bedrock, cliffs, and taws. <br />Parent material: residuum. <br />Rock type: igneous and metamorphic. <br />Runoff: rapid. <br />Cryaquolls <br />Effective rooting depth: greater than 40 inches <br />Drainage class: very poorly to somewhat poorly. <br />Depth to seasonal high water table: +t to 1 <br />feet. <br />Available water capacity: low to moderate. <br />Permeability: slow to moderately slow. <br />Runoff: medium. <br />VEGETATION <br />PotenBal natural communities: <br />Moran: kobresia(golden avenscurly sedge <br />(Koury/Acro-Caro) and tufted hairgrass/golden <br />avens (DecelAcro) and (Sagl1-Sabr1lDece) <br />moist site. <br />Cryaquolls: grayteaf willow-willow/sedges <br />(Sagl1-BALI/CARE) stream drainages and <br />(Caaq/Gaul) seeps and bogs and BaRic <br />rush/sedges (Juan/CARE) bogs. <br />Seral stages: dominated by plants of the <br />respective potential natural communities. <br />Present vegetat/on: dominated by plants of the <br />respective potential natural communities. <br />USE AND MANAGEMENT CONSIDERATIONS <br />Major uses: recreation, scenic vistas, wiMlife <br />habitat, and watershed. <br />Mass movement potential: <br />Landslides: low. <br />Debris flows: low. <br />Snow avalanche: low. <br />Sediment delivery efficiency: high. <br />Road and trail limitations: <br />Cut and fill slope stability <br />Moran; slight. <br />Rock outcrop: slight- cliffs and talus. <br />Cryaquolls: severe- high water table. <br />Improved unsurfaced roads: <br />Moran: slight. <br />Rock outcrop: severe- cliffs and talus. <br />Cryaquolls: severe- high water table. <br />ONroad vehicle roads and trails; <br />Moran: severe- erosion hazard. <br />Rock outcrop: severe- cliffs and talus. <br />Cryaquolls: severe- high water table. <br />Foot trails and paths: <br />Moran: slight. <br />Rock outcrop: severe- cliffs and talus. <br />Crvaauolis: severe- hioh water table. <br />