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Table 5-1 <br />DEIS Comments and Responses <br />Commenter Comment Comment/Response <br /> <br /> areas of 1 to 50 acres (PL LXVI, B, photo pairs for comparison of 1898 and <br /> 2003 are in the project file). <br /> The brushy forms are slender and from 2 to 12 feet high. Tree forms range <br /> from 4 to 10 inches in diameter, and frequently 14 to even 24 inches, while <br /> the common height is 12 to 25 feet. Growths of this kind were found only on <br /> the west slope of Hubbard Creek Basin and on the west side of the middle <br /> course of West Muddy Creek. Occasional thickets of much smaller trees <br /> occur on some of the rich, narrow benches in the region of Wallace Creek, on <br /> the north side of Battlement Mesa. <br /> While it is stated above, the brushy form of this species furnishes a generally <br /> conspicuous cover between the sage lands of the lower valleys and the lower <br /> levels at which the aspen occurs, it is becoming much more conspicuous in <br /> some of the broad interior basins. The high benches on the head waters of the <br /> Upper Gunnison River, West Muddy Creek, Hubbard Creek and Divide Creek <br /> are instances in which the vast areas covered by this brush deeply impress the <br /> observer." <br /> Even though this was written 109 years ago, Sudworth's comments pretty <br /> well characterize the status and condition of oak brush in this area today. <br /> However, it is now recognized that oak brush has more value than Sudworth <br /> mentioned. It does provide a variety of habitat for a variety of wildlife <br /> species, including big game and birds. Its value for wildlife is for cover, <br /> forage and browse. As a result a variety of age classes and structure provides <br /> the most benefits to wildlife. <br /> Sudworth also noted there were vast expanses of oakbrush in 1898, shortly <br /> after the Battlement Mesa Forest Reserve was established (December 24, <br /> 1892). Oak brush is probably located on the same sites on which they were <br /> located in 1898. However, as Paonia RD studies of historic photographs have <br /> shown, all woody vegetation on the GMUG NF is older, taller and denser; <br /> (Bradford et al. 2007) This has probably been caused primarily by fire <br /> suppression. Wildfire appears to have been a significant influence on the <br /> vegetation of the GMUG NF prior to American settlement. Sudworth noted in <br /> his Report on Battlement Mesa Forest Reserve p. 222 - 232, that "Forest fires <br /> have been very prevalent throughout the reserve." He noted that parts of the <br /> reserve appeared to have burned in 1878- 79, with less extensive burning <br /> taking place in 1883-85 and 1890-92. During the summer/fall of 1898 fires <br /> burned in August -October, with approximately 70,000 acres burning or 8 <br /> percent of the total reserve. In fact Sudworth photographed a number of sites <br /> that were actively burning or had burned earlier that season (Bradford et al. <br /> 2007 ). Analysis of over 300 historical photographs in the reference show that <br /> there is more woody vegetation today than at the time the GMUG MFs were <br /> established (1892, 1905 and 1905). This increase is due primarily to wildfire <br /> suppression. <br /> The Forest has used a variety of treatments to manage oak brush for various <br /> wildlife values, including prescribed fire and a variety of mechanical <br /> techniques including chaining, roller-chopping, and hydro-axing. In addition <br /> there has been other mechanical work, such as ushing rights-of--way for <br />• <br />• <br /> <br />164 Deer Creek Ventilation Shaft and E Seam Methane Drainage Wells FEIS <br />