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<br />temperatures to make the High Uintas a harsh environment for plant <br />growth. The low plant productivity of the interior of the range is a <br />consequence of the inhospitable environment. <br />Limestone and shales are currently confined to the edges (par- <br />ticularly the western flank) of the range. Deciduous forest of aspen <br />and thickets of oak are widespread above 1,900 m on limestones and <br />calcareous shales, but coniferous forest and alpine herblands dominate <br />the interior of the range where soils are derived from quartzite. <br />.,.;~ <br /> <br />VEGETATION <br />The vegetation of the Uintas above 2,135 m is dominated by forest <br />(Table 1-1) with coniferous forest prevailing above 2,740 m. Roughly <br />60% of the coniferous forest is dominated by lodgepole pine, the most <br />widespread vegetation type in the Uintas. Large areas of Engelmann <br />spruce and subalpine fir also occur in the range. Ponderosa pine is <br />less common in the area and is largely confined to the east and south <br />slopes of the range. Douglas fir forms stands locally throughout the <br />range, usually on limey outcrops. <br />Wet drainage bottoms and poorly drained valley bottoms in the <br />forested areas support verdant and moderately productive subalpine <br />meadows and willow thickets, the chosen habitat of the moose which has <br />recently invaded the area and established breeding populations. Above <br />3,350 m, forests are reduced to tangles of twisted, shrub-sized conifer <br />trees or disappear completely. The gentler slopes at high elevation <br />support alpine herblands that only locally consist of a species complex <br />that merits the name alpine tundra. <br />The flora of the Uintas is rich consisting of over 1,050 vascular <br />plants, 140 mosses and l~verworts, at least 40 species of lichen, 235 <br /> <br />6 <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />