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IIIIIIIIIIIIIIIIIII • ,-z~-~ ~ • <br />lj~~:EXHIBIT I <br />SOILS INFORMATION <br />Affected lands for the Yankee Gulch Project include the solution mining well field and <br />the initial processing plant area at the Piceance Site, a 50-foot-wide permanent corridor <br />along the 44-mile-long pipeline route, and the final processing plant area at the <br />Parachute Site. Soils are described in soil surveys conducted by the USDA Soil <br />Conservation Service (SCS). The Soil Survey of Rio Blanco County Area Colorado (SCS <br />1982) and the Soil Survey of Rifle Area Colorado (SCS 1985) provide detailed <br />information on the physical and chemical characteristics of soils within the affected <br />lands. Soil characteristics, including soil salvage and reclamation characteristics, are <br />summarized below for soil mapping units within the affected lands. <br />Soil conditions within the affected lands are highly variable due to differences in the <br />soil-forming factors: parent material, topography, vegetation, and climate. The semi- <br />arid environment of the resource area has affected soil development. Lack of moisture, <br />cool nights, a:~d infrequent high temperatures suppress vegetation growth and slow the <br />chemical and biological processes needed for good soil development. In addition, <br />geologic erosion has progressed too rapidly for many soils to develop distinct deep <br />horizons (BLM 1994). Soils in the Piceance Creek Basin occupy varying landforms <br />including drainageways and narrow valleys, rolling hills, and high mountains with <br />very steep side slopes. Slopes range from 0 to 90 percent. Soils are shallow to deep and <br />have formed in alluvium, colluvium, residuum, and reworked eolian deposits derived <br />predominantly from shale and sandstone (SCS 1982). Native vegetation ranges from <br />streambank riparian shrub communities along perennial streams to sagebrush <br />communities that occur at all elevations, mountain shrub communities at higher <br />elevations, and pinyon-juniper communities on shallow soils on mountainsides and <br />ridges. Major uses include wildlife habitat and livestock grazing. <br />Soils are considered fragile when they exhibit the following criteria: <br />• Areas rated as highly or severely erodible by wind or water, as described by the <br />SCS. <br />• Areas with slopes greater than 35 percent if they have one or more of the <br />following soil characteristics: (a) surface texture that is sand, loamy sand, very <br />fine sandy loam, fine sandy loam, silty clay or clay, (b) a depth to bedrock that is <br />less than 20 inches (described as shallow or very shallow), (c) an erosion <br />condition that is rated as poor, or (d) a K (erosion potential) factor of greater than <br />0.32 (BLM 1994). <br />Site-specific information related to the general soil type, thickness, distribution of soils <br />over the affected land, and suitability of topsoil for establishment and maintenance of <br />I-1 <br />