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Fremont County Area, Colorado <br />and swelling of the soil around foundations has been <br />reduced in most areas because seepage and former <br />crop irrigation have moistened the soil, and irrigation of <br />lawns helps to maintain a constant soil moisture <br />content. Basements are not suitable in most areas <br />unless the seepage.from irrigation water is drained. <br />Conventional septic tank absorption fields do not <br />function adequately because of the restricted <br />permeability. Other types of sewage disposal systems <br />may be needed. The seasonal high water table also <br />generally makes conventional systems unsuitable. <br />The capability classification is Ills, irrigated, and Vls, <br />nonirrigated. The unit is in the Salt Flat #34 range site. <br />64=Louviers-Travessilla complex, 20 to 50 percent <br />slopes. These soils are on hills, ridges, hogbacks, and <br />canyonsides. The native vegetation is mainly pinyon <br />and juniper. Elevation is 5,300 to 6,800 feet. The <br />average annual precipitation is 13 to i5 inches, the <br />average annual air temperature is 48 to 52 degrees F, <br />and the average frost-free period is 120 to 150 days. <br />This unit is about 40 percent Louviers soil and 35 <br />percent Travessilla soil, The Louviers soil is on side <br />slopes and on the scarp side of hogbacks. The <br />Travessilla soil is on canyon rims, ridges, and the upper <br />part of side slopes and in areas of weather-resistant <br />bedrock on hogbacks. <br />Included with these soils in mapping are areas of <br />sandstone rock outcrop on ridges, canyon rims, and <br />side slopes. These areas make up about 5 percent of <br />the unit. Also included are areas of moderately deep, <br />clayey soils on side slopes. These included soils make <br />up about 5 percent of the unit. Areas of the deep <br />Cascajo soils are on the crest of side slopes and on <br />foot slopes. These soils have a surface layer of very <br />gravelly sandy loam. They make up about 5 percent of <br />the unit. Also included are areas of the deep Kim and <br />Otero soils in drainageways. Kim soils have a surface <br />layer of loam. They make up about 5 percent of the <br />unit. Otero soils also make up about 5 percent of the <br />unit. They have a surface layer of sandy loam. A few <br />small areas of gypsum land are along the south edge of <br />Sixmile Park. <br />The Louviers soil is shallow and well drained. It <br />formed in residuum derived dominantly from shale and <br />siltstone. The surface layer is typically light brownish <br />gray very channery clay loam about 3 inches thick. The <br />substratum is mainly clay about 13 inches thick. Shale <br />bedrock is at a depth of about 16 inches. The soil is <br />neutral to a depth of 3 inches. It is mildly alkaline to a <br />depth of 6 inches and is neutral below that depth. In <br />some areas the soil is calcareous and moderately <br />alkaline. In other areas the surface layer is very cobbly <br />or very stony. <br />55 <br />Permeability is slow in the Louviers soil. Available <br />water capacity is very low. Effective rooting depth is 10 <br />to 20 inches. Runoff is very rapid, and the hazard of <br />water erosion is very high. <br />The Travessilla soil is shallow and well drained, It <br />formed in residuum derived dominantly from sandstone. <br />The surface layer is typically light brown channery loam <br />about 4 inches thick. The substratum is channery loam <br />about 10 inches thick. Sandstone bedrock is at a depth <br />of about 14 inches. The soil is moderately alkaline. <br />Permeability is moderate in the Travessilla soil. <br />Available water capacity is very low. Effective rooting <br />depth is 4 to 20 inches. Runoff is rapid, and the hazard <br />of water erosion is very high. <br />This unit is used as noncommercial woodland, for <br />livestock grazing, or for wildlife habitat. Livestock have <br />limited access to the steeper areas because of the <br />slope, and thus overgrazing is a concern in the less <br />sloping areas. <br />The potential plant community is mainly pinyon and <br />juniper and an understory of Scribner needlegrass, <br />western wheatgrass, blue grams, sideoats grams, <br />Gambel oak, and mountainmahogany. The potential <br />production of native understory vegetation in normal <br />years is about 300 pounds of air-dry vegetation per <br />acre. If the condition of the understory deteriorates, red <br />threeawn, blue grams, pricklypear, and other forts and <br />shrubs increase. <br />Woodland products, such as firewood, fence posts, <br />Christmas trees, and pinyon nuts, are produced in <br />areas of this unit. Generally, only the foot slopes and <br />ridges are accessible. The slope limits harvesting in <br />other areas. The use of tree spades for removal of <br />transplants is severely limited. <br />Thinning the overstory generally enhances <br />reproduction and promotes the growth of grass and <br />younger trees. After pinyon and juniper are thinned or <br />harvested, seeding grasses reduces the hazard of <br />erosion. Deferring grazing in harvested areas for at <br />least 2 years ensures the development of a plant cover <br />that is sufficient to protect the soils from erosion. <br />This unit is poorly suited to homesite development. <br />The main limitations are the slope and the depth to <br />bedrock. <br />The capability classification is Vlle, nonirrigated. The <br />unit is in the Pinyon-Juniper woodland site.. <br />65-Manvel silt loam, 0 to 3 percent slopes. This <br />deep, well drained soil is on plains, foot slopes, fans, <br />and stream terraces. It formed in alluvium derived from <br />limestone and shale. The native vegetation is mainly <br />grasses. Elevation is 5,000 to 5,300 feet. The average <br />annual precipitation is 12 to 14 inches, the average <br />annual air temperature is 51 to 53 degrees F, and the <br />