Laserfiche WebLink
2.04.10 Vegetation Information <br />DENSITY <br />Shadscale is the most abundant shrub in this vegetation type with a density of <br />1,790 shrubs per acre. Broom snakeweed is also common with 881 shrubs per acre. <br />Total shrub density is 2,987 shrubs per acre. Average shrub height for all shrubs is 51 <br />centimeters. See Table 4.5.9. <br />RICHNESS AND EQUITABILITY <br />Of the three vegetation types sampled, species richness is lowest in the <br />Shadscale Shrubland (index = 11.90). This is probably related to the harsh <br />environmental conditions existing on these steep slopes. Equitability is also relatively <br />low (index = 0.73). See Table 4.5.6. <br />JUNIPER WOODLAND <br />Juniper Woodland occurs on the steep, north and west facing slopes and the <br />ridgetops surrounding the McClane Mine. This vegetation type occurs mainly on the <br />Torriorthent rock outcrop complex although there are inclusions of Havre loam, a deep, <br />well drained soil. Juniper Woodland is the climatic climax for these environmental <br />conditions. <br />COVER <br />This vegetation type contains 41 species of plants. These include: 2 trees, 12 <br />shrubs and subshrubs, 11 graminoids, 14 forbs, and 2 succulents. Tree cover <br />dominates with 26.0 percent cover. Total vegetation cover is 45.3 percent. Litter, soil, <br />and rock are relatively abundant with 23.3, 17.0, and 14.5 percent cover, respectively. <br />See Table 4.5.10. <br />Utah juniper is the dominant tree species providing 20.8 percent cover. Pinyon <br />pine Pinus edulis also common to a lesser degree (5.3 percent cover). <br />Major graminoids in this woodland are: Salina wildrye (6.3 percent cover), Indian <br />ricegrass (2.0 percent cover), and mutton -bluegrass, Poa fendleriana (2.0 percent <br />cover). Minor grasses are cheatgrass and Sandberg bluegrass. <br />Shrub cover is relatively sparse, but more common shrubs are mountain <br />mahogany, Cerococarpus montanus (5.3 percent cover), and Gamble oak, Guercus <br />PR -02 2.04-63 10/12 <br />