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Northam San isabed erW Vyestcvn Pike Netionaf forests. Colorado <br />TYPICAL PROFILES: <br />Moran <br />Surface layer(s): <br />0 ro 2 inches -dark grayish brown, gravely <br />sandy loam. <br />2 ro 10 inches -brown, gravelly sandy bam. <br />Subsoil layer(s}: <br />10 to 20 inches - yeflowish brown, very graveity <br />sandy loam. <br />20 to 32 inches -light yellowish brown, very <br />cobbiy sandy loam. <br />Substratum layer(s): <br />32 ro 60 inches -light olive brown, very cobbty <br />sandy loam. <br />Cryaquolis <br />Surface covering layer. <br />4 ro 0 inches -dense mat of partly decomposed <br />vegetation. <br />Surface Layer(s): <br />0 to 12 inches -black, sift loam. <br />12 to 18 inches -black, very gravetty sift loam. <br />Substratum layer(s): <br />18 to 60 inches -dark greenish gray, very <br />gravely sandy foam. <br />Histosola <br />Surface layer(s): <br />0 ro 10 inches -slightly decomposed plant roots <br />and other organic material. <br />Subsurface layer(s): <br />10 to 24 inches -slightly decomposed plant <br />roots. <br />24 ro 35 inches - partially decomposed plant <br />roots. <br />Substratum layer(s~: <br />35 to 40 inches -dark grayish brown silty clay <br />loam. <br />40 to 45 inches -dark grayish brown sandy clay <br />foam. <br />45 inches -weathered gneiss and schist. <br />SOIL PROPERTIES AND QUALfTiES <br />Moran <br />Effecdrre rooting depth: greater than 60 inches. <br />Drainage class: somewhat excessively. <br />Depth to seasonal high water table: greater <br />than 6 feet. <br />AvaUablewatercapacity; low. <br />Permeability: moderately rapid. <br />Runoff: medium. <br />Cryaquolls <br />Effective rooting depth: greater than 60 inches. <br />Drainage class: very poorly ro somewhat poorly. <br />Depdt M seasonal high water table: +1 to 1 <br />feet. <br />Available water capacity: low ro moderate. <br />Permeability: slow ro moderately slow. <br />Runoff: medium. <br />Histosols <br />Etfectlve rooting depth: greater than 40 inches. <br />Drainage class: poorly. <br />Depth to seasonal hdgh water table: +1 to 1 <br />feet <br />Available water capacity: low. <br />Permeability: slow. <br />Runoff: slow. <br />VEGETATION <br />Potential natural communities: <br />Moran: kobresia/golden avens-curry sedge <br />(KomyJAcro-Caro) and tufted hairgrass/golden <br />avens (Dace/Acro) and (Saglt-Sabr1lDece) <br />moist site. <br />Cryaquolis: grayleaf willow-willowlsedges <br />(Sagl1-SALT/CARE) stream drainages and <br />water sedge/beaked sedge (CaaglGaut) seeps. <br />Histosois: water sedgelbeaked sedge <br />(CaagJCaut) seeps and Baltic rushlsedges <br />(Juar/CARE} bags. <br />Seral stages: dominated by plants of the <br />respective potential natural communities. <br />Present vegetation: dominated by plants of the <br />respective potential nalural communities. <br />USE AND MANAGEMENT CONSIDERATIONS <br />MaJor uses: recreation, scenic vistas, wildlife <br />habitat, and watershed. <br />Mass movement potential: <br />Landslides: tow. <br />Debris flows: low. <br />Snow avalanche: bw. <br />Sediment delltrery efticfency: high. <br />Road and trail Ilmitations: <br />Cut and fill slope s[ability <br />Moran; stighE_ <br />Cryaquolis: sevem- high water table and <br />saturated soil. <br />Histosols: severe- high water table and <br />organic materials. <br />improved unsurfaced roads: <br />Moran: slight. <br />Cryaquoiis: severe- high water table and <br />saturated soil. <br />Histosols: severe- high water table and <br />organic materials. <br />Of/road vehicle roads artd trails: <br />Moran; severe- soil erosion, surface <br />compaction, and rutting. <br />Cryaquoiis: severe- high water table and <br />saturated soil. <br />Hlstosols: severe- high water table and <br />organic materials. <br />