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-14- <br />• RESULTS AND DISCUSSION <br />Those studies dealing with the entire study area, exclusive of individual <br />vegetation types are presented first. These include vegetation type <br />mapping and vegetation species composition. Baseline vegetation data <br />such as tree density and basal area, cover, frequency, productivity and <br />shrub heights gathered >n different vegetation types on Nucla Mine are <br />presented below. A description of the major vegetation parameters <br />measured and an evaluation of samq~ling adequacy concludes the report sec- <br />tion. Raw and analyzed data are provided on computer printouts in Appen- <br />dix B. Summary tables are utilized in the text where appropriate. <br />Weather wnditions within a given year, notably the amount and monthly <br />distribution of precipitation, can have a considerable effect on certain <br />vegetation parameters, especially productivity which, during unusually <br />• wet years, may increase dramatically. Therefore, in the interest of <br />qualifying the vegetative data base presented in the report for the <br />1979 growing season, precipitation data gathered at a nearby weather sta- <br />tion are included for the 1979 givwin4 season and for the six tronths <br />preceeding the 1979 growirxJ season (Table 2). Precipitation data for the <br />six month period prior to the growing season is important because the <br />amount and distribution of precipitation during this period influence <br />total soil moisture and thus, the amount of moisture available to plants <br />during the following growing season. <br />VDC;FTATIVE TYPE MAPPING <br />Delineation of vegetation types on the study area is depicted on Map 1, <br />("Vegetation Types"), Appendix A. Phe total acreages of each mapping unit <br />shown on Map 1 are surmiarized >n Table 3. <br />VEGETATION SPDCIES COMPOSPI'ION <br />~. A listing by life form of all vegetative species encountered on or near <br />the study area is presented in Apperrlix C. A total of 132 species have <br />