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<br />• The beginning of the pipeline route, which lies within the Piceance Site, traverses <br />all five of the upland plant communities described for the Piceance Site, above (see <br />Figure 7-17). Immediately upon exiting the Piceance Site, the pipeline route crosses <br />the cultivated hayfields that occupy the Piceance Creek valley bottom. On the east <br />side of Piceance Creek and Piceance Creek Road, the pipeline route ascends Davis <br />Gulch. The bottom of Davis Gulch is occupied by sagebrush vegetation. As the <br />pipeline route comes up out of Davis Gulch and begins to follow the existing east- <br />west Questar natural gas pipeline corridor, it crosses barren/rock outcrop vegetation <br />that occupies the Thirteenmile Creek Tongue of the Green River Formation at this <br />location. The upland areas from this point to the Greasewood Compressor Station <br />primarily support open pinyon-juniper woodlands. <br />The second pipeline corridor segment includes approximately 11 miles of BLM land <br />paralleling the existing north-south pipeline corridor and extending from the <br />Greasewood Compressor Station south to about 2 miles north of the Rio Blanco <br />County/Garfield County Line (in T4S, R96W, Section 3). Virtually all ridge and <br />upland communities in this segment support pinyon-juniper woodlands (BLM <br />1998d), for a total of 3 to 4 miles traversed (CIG 1995). This segment also crosses <br />between 5 and 6 miles of sagebrush vegetation and approximately 2 miles of the <br />Mountain Shrub Association (CIG 1995). The Mountain Shrub Association has been <br />described by the BLM as follows (BLM 1994). <br />• Mountain Shrub Association <br />The Mountain Shrub Association is a mixture of large to medium tree-like shrubs, <br />most often Gambel's oak, that have a mixed understory of smaller shrubs, grasses, <br />and forbs. The overstory varies from open to dense stands, and understory species <br />density and diversity are inversely related to overstory closure. In some areas, the <br />mountain shrub type supports the highest herbaceous production and species <br />diversity of any plant association. <br />The association occupies higher elevations on east, west, and north slopes, <br />extending to lower elevations on cool exposures. The primary environmental factor <br />affecting the Mountain Shrub Association is available moisture, as influenced by <br />elevation, soils, topography, and wildfire. It is largely restricted to elevations about <br />7,000 feet in higher precipitation zones. At lower elevations on deeper, well-drained <br />soils, the type commonly intergrades with the Sagebrush Association. Where it <br />occurs along the proposed pipeline corridor, it occurs primarily on ridgetops and on <br />east- and north-facing slopes (CIG 1995). <br />The third pipeline corridor segment includes approximately 24 miles of private land <br />paralleling the existing north-south pipeline corridor and extending from the <br />southern boundary of the BLM land south to the Parachute Site (in T6S, R96W, <br />Section 34). This segment traverses between 11 and 12 miles of sagebrush <br />• vegetation, 4 to 5 miles of mountain shrub vegetation, including the top of Davis <br />Point (in T5S, R96W, Section 24) (Barrett 1994), and less than 2 miles of pinyon- <br />American soda, L.L.P. '7_3rJ <br />Commerual Mine Plan <br />August 18, 1998 <br />