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Memo to Tony Waldron <br />Bowie No. 2 Geotechnical Adequacy <br />page 3 <br />difficult:y, reminiscent of the problems encountered by Mountain Coal while <br />facing up the F-seam portals of the Mountain Gunnison No. 1 mine. The resulting <br />engineE~red remedial construction cost several million dollars and was <br />margin<~Ily effective. The portals continue to evidence displacement fifteen <br />years later, necessitating continued remedial expenditures. <br />2.05.3(2) Operation Description - Underground Mining <br />The m~ijority of the following comments in this section apply uniformly to all <br />the proposed surface facilities at the Bowie No. 2 mine. <br />BRL included a facsimile of Raye Junge's Colorado Geological Survey Map 06), <br />and excerpts from it's accompanying text (Exhibit 12, Volume III) in the <br />application. Mr. Junge's map was entitled "Geologic Hazards in the Hotchkiss- <br />Paonia Reservoir Area, Gunnison and Delta Counties, Colorado". BRL presents its <br />proposed surface facilities on Maps 15-1 and 15-2 of the application. While <br />comparison is complicated by the significantly differing scales of maps 06 and <br />15-1 & 2, it appears that the majority of the proposed BRL surface facilities lie <br />within <~reas mapped by Mr. Junge as landslides. The vent shaft pads, the portal <br />bench, and the coal stockpile bench appear to lie within a recent landslide zone <br />(Ise). The conveyor, haul road and stockpiles lie within a larger and older <br />landslide zone (IsZ). The explanation to Mr. Junge's map explains these hazard <br />design~itions as follows. <br />"LANDSLIDE: A landform resulting from the moderate to rapid, downward <br />and outward movement of rock and/or soil where there is a surface or <br />zone of weakness that separates the landslide from more stable <br />underlying material. Landslides, including earthflows, result from the <br />rriass movement of rock and/or soil in response to gravitational stresses <br />and these movements may affect adjacent downslope areas. Natural and <br />man-caused disturbance of landslide areas could initiate <br />additional instability and mass movement. Relative age of <br />Iz~ndslides is indicated by subscripts (1 is the youngest)." [Emphasis <br />added] <br />