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• • Vegetation Information <br />about 1 % or 2% ground cover under the trees, and the remainder occupied by scattered shrubs. Although <br />about 90% of the ground surface is essentially bare in most places, erosion is slight. This is mainly due to <br />the highly organic soil that can absorb large amounts of water without eroding. <br />South Facing Slopes: <br />Map Unit Name: Pinon Pine/Juniper/Mountain Mahogany <br />General Description: Tn striking contrast to the north facing slopes, the south facittg slopes are <br />more like a desert grassland. The slopes aze generally steep and rocky and occupied by species that are <br />typically very drought resistant. Cactus (Prickly Pear and various "pincushion" cacti) are ccmmon and in <br />places form dense growths. Grasses are often abundant, except where the soil is very rocky. Most of the <br />vegetation cover is composed of grasses, fortis, and shrubs. Trees form a very minor component of the <br />vegetation and are often widely spaced or completely absent from large areas. This vegetation, although <br />characterized and visually dominated by trees and shrubs, would actually be called a shrubby grassland, if <br />numerical relationships are used to name the vegetation. Species diversity is very high, in fact, most of the <br />species found over the entire site are found on these south facing slopes rather than the north facing <br />slopes. The high species diversity is probably due to the extremely high degree of microem~ironmental <br />diversity on the south facing slopes. <br />In the shade of large rocks, rich growths of grass and even ferns can be found. Yet, a few feet away, <br />in an open, hot, dry site the vegetation may be dominated by stands of Prickly Pear cactus mixed with <br />Blue Grama and Western Wheatgrass, two typical prairie grasses. This prairie type growth may then <br />abruptly transition into a shrub dominated vegetation composed, usually, of Mountain Mahogany. <br />Occasionally blended with the Mountain Mahogany may be Gambel Oak, Antelope Bitterbrush, <br />Skunkbush, or Gooseberry. <br />The trees on these slopes are mostly Pinon Pine or Rocky Mountain Juniper, but occasional specimens <br />of One-seed Juniper can also be found. Near the crest of the slopes and occasionally in the mid-slope area, <br />Ponderosa Pine can also be found. Most of the trees are isolated from each other with separations (crown <br />edge to crown edge) of 50 to 100 or more feet. The space between the trees is occupied by the high <br />diversity grass, shrub, and forb communities. <br />Whete the north facing slope and south facing slope vegetation units meet in the bottom of the valleys, <br />the transition is usually very narrow. The Douglas Fir may extend a short distance (10 to 2~) feet in <br />elevation) up the south facing slope and Juniper and sometimes Pinon may extend a similar distance up <br />the notth facing slope. Ground cover in these transition areas is often nearly 100% and composed mainly <br />of Bluegrass (Poa), Bromegrass (Bromus), and other species common to more moist land neaz ephemeral <br />streams. These transition areas may also include Rocky Mountain Maple and River Alder, lwt the latter <br />two species aze only common locally. Chokecherry can be found in the valley bottoms and growing a <br />short distance up adjacent slopes. <br />As mentioned previously, the slope crests where the south facing and the north facing vegetation meet <br />is characterized by a mixture of Ponderosa Pine, Douglas Fir, Gambel Oak, and a blend of various ground <br />level species common to each of the vegetation units. This transition is similar in structure to the transition <br />Menzer Quarry Amendment Exhibit J Page 4 <br />