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C~ <br />• <br />2 <br />black-footed ferret were not uncommon in large prairie dog towns (Armstrong <br />1.972). All are no longer resident within the state. Although extinctions of bird <br />species are not recorded, the plains sharp-tailed grouse has been extirpated from the <br />~zciniry (Braun et al. 1992), Fortunately, most species have not suffered so <br />extensively, but many have been reduced in numbers -- some significantly. Many <br />plant species not native to this area have become established and in some cases <br />dominant, especially in areas that historically or currently are to some degree <br />disturbed by human activity (including livestock grazing, alteration of natural <br />processes such as fire or flooding, gravel muting, agricultural activity, road building <br />or other development). [t is within the purpose of this effort to identify the <br />conservation sites which will protect the most sensitive element of natural diversity. <br />Climate. The climate of the area is strongly influenced by the mountains and <br />is continental in character. Sudden and extreme changes in atmospheric conditions <br />rtay occur from hour to hour and day to day at any season of the year. The <br />average wind velocity is moderate, although strong gusts (occasionally over 80 <br />r-tph) are not infrequent (U. S. Dept. of Energy 1980). Winters are generally cool <br />and dry and summers warm. The mean first date of frost is October ?and the mean <br />last day of frost is May 9. Average yearly precipitation for the period from 1953- <br />1976 is approximately 15 inches (U. S. Dept. of Energy 1992). Approximately 70% <br />cf the moisture falls during the growing season, mostly in late spring and early <br />summer (U. S. Dept. of Energy 1992, U. S. Dept. of Agriculture 1980). <br />Soils. Soils are of two major types. Soils on terraces or piedmonts are a <br />stony or skeletal type developed on glacial outwash (Rocly Flats Alluvium). Fine <br />t.=xtured soils developed from shales and mudstones are common in the small <br />drainages associated with Rock Creek (U. S. Dept. of Agriculture 1980). <br />Geology. Geology is discussed in detail in several papers or reports from the <br />area (U. S. Dept. of Energy 1992, Branson et al. 1965, Vestal 1919) and is an <br />imponant factor influencing the distribution of plant communities. <br />(:olorado's Natural Heritage Program <br />To place this report in context it is useftil to understand the history and <br />fimctions of the Colorado Natural Heritage Program (CNHP). CNHP has been <br />extant in Colorado For 16 years. CNHP was relocated from the Division of Parks <br />and Outdoor Recreation into the University of Colorado Museum in the spring of <br />1992, and more recently to the College of Natural Resources at Colorado State <br />University. With an increased staff, the Program is revitalized and updating <br />comprehensive information on the rare, threatened, and endangered species and <br />significant natural communities in Colorado. The mtilti-disciplinary team of <br />scientists and information managers gather information and incorporate it into <br />