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i <br />CNAP~ERTHREE Affected Em~ironment <br />largely restricted to elevations about 7,000 feet in higher precipitation zones. At lower elevations <br />on deeper, well-drained soils, the type commonly intergrades with the Sagebrush Association. ' <br />The overstory vanes from open to dense stands, and understory species density and diversity aze <br />inversely related to overstory closure (BLM 1994). Where it occurs along the proposed pipeline <br />corridor, the Mountain Shrub Association occurs primarily on ridgetops and on past- and north- <br />facing slopes (BLM 1998c). This community is used extensively as wildlife habitat for mule <br />deer and grouse from late spring to late fall (SCS 1982). ' <br />The Mountain Shrub Association is a mixture of large to medium tree-like shrugs, most often <br />dominated by Gambe] oak. A mixed understory of smaller shrubs includes snowberry, <br />serviceberry, and Woods rose. The most common grasslike species are various :>edges. <br />American vetch, bedstraw, Colorado columbine, and lambsquarter aze common .forbs. In some <br />azeas, the mountain shrub type supports the highest herbaceous production and species diversity <br /> <br />of any plant association. ' <br />The third pipeline corridor segment includes approximately 22 miles of private land paralleling <br />the existing north-south pipeline corridor and extending from the southern boundary of the BLM <br />land south to the Parachute Site. This segment traverses about 11 miles of sagebrush vegetation, <br />4 miles of mountain shrub vegetation, including the top of Davis Point (Barrett 1994), and less <br />than 2 miles ofpinyon-juniper woodlands (CIG 1995). In a few places, aspen sningers or stands <br />approach the pipeline corridor between MPs 27 and 28, and small areas of Douglas-fir forest are <br />crossed neaz MPs 14 and 20 (BLM 1998c). Batren/rock outcrop vegetation occupies the ' <br />ridgeline at Davis Point (Barrett 1994). The pipeline corridor also crosses about 5 miles of <br />agricultural land, including a small amount of irrigated land along Parachute Creek north of the <br />Parachute Site (CIG 1995). A few riparian wetland communities in the study area occur as <br />narrow bands associated with Piceance Creek and Parachute Creek (Steigers 1998b). <br />Agricultural Land ~ a <br />Agricultural lands aze found along valley bottom lands, primarily along Stewart Gulch, Piceance <br />Creek, and Parachute Creek. Agricultural land is a man-made community that consists of hay <br />meadows and natural vegetation interfaces. Common species include alfalfa, clover, wheatgrass, <br />Kentucky bluegrass, red-top, brome, and orchard grass. Some of the fields are irrigated or <br />flooded by ditches along the valley bottom. <br />Riparian and Wetland Vegetation , <br />Riparian vegetation in the area is dominated by grasses, including western wheatgrass, slender <br />wheatgrass, and needlegrass, as well as several sedges and rushes. Shrubs, including big <br />sagebrush, rubber rabbitbrush, and greasewood, are present but sparse (BLM 198:!). This <br />community occurs south of the Piceance Site along Piceance Creek, where it occupies Hagga <br />loam and Havre loam soils and typically is used extensively for winter range for mule deer. <br /> <br />Pazachute Creek and its tributaries typically support box elder and narrowleaf cottonwoods in the ' <br />overstory. Understory vegetation is vaned but typical species include sandbar willow, <br />serviceberry, chokecherry, and skunkbrush (Steigers 1998a). Riparian vegetation in the vicinity <br />of Parachute Creek occupies torrifluvent soils (alluvial soils on floodplains). These riparian <br />3-30 Vegetation ' <br />