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NE PA COMPLIANCE <br />COLORADO WESTMORELAND INC. <br />RIGHT-OF-WAY APPLICATIONS FOR <br />,,'~~ ORCHARD VALLEY WEST MINE Page -4- <br />bitterbrush, big sagebrush, pinyon, Utah juniper, true mountainmahoga- <br />ny, stiff goldenrod, mountain pepperweed, cheatgrass, bedstraw and elk <br />sedge. No threatened or endangered plant or animal species are known <br />to exist in the area. As identified in the Uinta-Southwestern Utah <br />Coal Re ion Round Two Final EIS, October, 198 t e area s nterm e- <br />diate to crucia deer and a winter range and actual densities vary <br />with the severity of the winter. The site is part of the Steven's <br />Gulch grazing allotment. <br />The area has been inventoried for cultural resources and none were <br />identified, Suspected Indian game blinds on the Fry Mesa ridge were <br />test excavated and found to be insignificant, Soils of the access road <br />and telephone line were identified in the USDA, Soil Conservation Ser- <br />vice, Soil Surve of Paonla Colorado, January, 1981, as Delson very <br />stoney oam, 20% to 60% s opes. T ese soils are deep and well drained <br />with an 8" thick dark brown very stoney loam surface layer, Subsoil is <br />reddish brown stoney clay and about 34" thick, The substratum is pale <br />brown very stoney clay loam about 60" in depth. <br /> <br /> <br />In addition to Delson very stoney loam, the 46 KV powerline would cross <br />three soil types: Cerro stoney loam, 10% to 35% slopes; Delson stoney <br />loam, 3% to 20% slopes; and Torriorthents-Rock outcrop, sandstone com- <br />plex. Delson stoney loam differs from Delson very stoney loam in that <br />it is generally found on less steep slopes and contains fewer stones. <br />Cerro stoney loam soils are deep, well drained, with a 6" surface layer <br />of brown stoney loam, a 25" subsoil layer of reddish brown clay and a <br />60" thick substratum of pink gravelly clay loam. Torriorthents soils <br />are well drained, have a loamy, very stoney surface layer and underly- <br />ing layers are sandy loam with a high content of rock fragments. <br />The areas of the road, telephone line and powerline are rated as YRM <br />Class III. The terrain of the area is already disrupted by the `Blouch <br />Road", Steven's Gulch Road and CWI's existing powerline, The area is <br />in the background from major points of observation. <br />IV, ENVIRONMENTAL CONSEQUENCES <br />A. PROPOSED ACTION <br />"w <br />~ • <br />The proposed expansion of the "Rlouch Road" including road sur- <br />face, cuts and fills, from Steven's Gulch Road to the Lease <br />qC-37210 boundary, would disturb less than three additional acres <br />of public lands and loss of vegetation. The largest fill would <br />extend approximately 110' downslope. Cut materials not utilized <br />for road fills will be included in the fill constructed at the <br />Orchard Valley West Mine bench, No side cast construction tech- <br />niques, resulting in damage to downslope vegetation, will be <br />