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<br /> <br />regions of Northwestern Colorado. They represent soils that grade from <br />recently developed soil bodies with minimum horizon development (F.ntisols) to <br />older soils with well-defined diagnostic horizons (Mollisols). <br />Overall, the soils found in the proposed permit area are relatively deep and <br />fairly well-drained. Effective rooting depth varies from two to sixty inches <br />within the area. The deepest soils yielding the greatest rooting depths occur <br />within valleys and on the leeward side of ridges. Soil reaction is slightly <br />acid to moderately alkaline over the permit area with the exception of <br />inclusions of small scattered areas with saline substrata. These small areas <br />have probably formed in place from weathered sodic shales. <br />Vegetation in the area grows largely in response to macro climatic influences <br />of the region. The north-facing slopes, having moderate to deep soils, a <br />relatively me sic moisture regime, and favorahle levels of insolation <br />throughout the year are characterized by well-developed mountain shrub <br />communities. On the colluvial toe-slopes, communities dominated by sagebrush <br />and some grasses occur. On the south-facing slopes behind the ridgeline of <br />the Williams Fork mountains, vegetative communities are not as well-developed <br />in terms of cover, density and production due to the less favorable soils, <br />moisture regime, and increased solar insolation. The trend in these areas is <br />toward communities dominated by juniper, pinyon, mountain mahogany and <br />xerophytes. <br />Within the permit area, natural vegetative communities have heen modified to <br />varying degrees by man and domestic animals. Much of the land along <br />toe-slopes and valley bottoms has been cleared of native vegetation and is <br />currently utilized for dryland agriculture. Most of the north-facing slopes <br />in the area have been historically used for the grazing of sheep and/or <br />cattle. Due to the above, the permit area is characterized by a mosaic <br />distribution of communities. <br />In transversing the permit area from east to west, the mountain shrub <br />community begins to thin (in terms of density and cover) until it is replaced <br />on the far west by a community of big sagebrush and grasses. Oescendina from <br />the ridge of the Williams Fork Mountains (proceeding northward), several <br />changes in community composition are noted. At elevations above 7,200 feet, <br />the mountain shrub community is characterized by Gambel's oak, which is <br />dominant over serviceberry and chokecherry, Snowberry is the most conspicuous <br />understory component, with an occasional big sagebrush, rubber rabbitbrush, or <br />bitterbrvsh. With a decrease in elevation comes a corresponding decrease in <br />oak dominance. Sagebrush, serviceberry and chokecherry are interspersed, <br />while oak dominates only in east-facing slopes. Entering the lowest <br />elevations, the serviceberry/chokecherry component diminishes, leaving a <br />community dominated by sagebrush, rabbithrush, and grasses. <br />Due to the presence of many and varied habitat types, many types of fauna are <br />found in and adjacent to the permit area. Antelope are found year round in <br />the lower sagebrush and cropland areas. Mule deer are found in the mountain <br />shrub community, sagebrush/grass community and pinyon/juniper community (to <br />the south of the permit area) during all seasons of the year. Elk use the <br />permit area primarily in the fall, winter, and early spring. In the summer <br />-8- <br />