Laserfiche WebLink
2.04.9 <br />Because steepness of slope, this soil is unsuited to crops, and reseeding of <br />depleted or destroyed native vegetation is not feasible by conventional <br />methods. A fair degree of success can be expected by broadcasting seed of <br />nonirrigated grasses in spring orfall. Pubescent wheatgrass, smooth brome, <br />and crested wheatgrass are adapted grasses. Good pasture management <br />should be practiced to maintain the grasses. <br />The potential plant community on this soil consists mainly of wheatgrasses, <br />bluegrasses, and needle - grasses. As range condition deteriorates, <br />wheatgrasses and needlegrasses decrease, forbs and woody shrubs <br />increase, and undesirable weeds and annual plants invade and become <br />more abundant. <br />This soil is used for winter range by mule deer and elk. Some important <br />plant species which can be managed for optimum production are bitterbrush, <br />mountainmahogany, Gambel oak, serviceberry, and elk sedge. Berry- <br />producing shrubs are an important habitat element of black bear. This soil <br />provides habitat for Merriam turkey, blue grouse, and band - tailed pigeon. In <br />favorable years, nature Gambel oaks produce acorns, which are used by <br />Merriam turkey. <br />41 — Fughes- Curecanti stony loam 10 to 40 percent <br />These strongly sloping to steep soils formed in glacial outwash, landslide <br />deposits, and old alluvial fans. Elevation ranges from 6,500 to 8,500 feet. <br />Average annual precipitation is about 18 inches, average annual air <br />temperature is about 42 degrees F, and the average frost -free season is <br />about 100 days. <br />Included with these soils in mapping are a few small areas of Cochetopa and <br />Bulkley soils and areas of Cryoborolls, very stony. Slips and slides are <br />common, especially in disturbed areas. The included soils make up 20 <br />percent of the complex. <br />The Fughes soil is deep and well drained. It formed in old alluvial fans and in <br />landslide deposits derived from sedimentary rock. <br />PR-14 2.04-99- 03/14 <br />