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Land Use and Cultural and Historic Resource Information - <br />Detailed information regarding land uses and cultural and historic resources within the Bowie No. 2 Mine <br />permit area is provided in Sections 2.04.3 and 2.04.4 of the permit application document. Abrief summary <br />is provided below, and this summary is derived from the information presented within Sections 2.04.3 and <br />2.04.4 of the permit application document. <br />The Bowie No. 2 Mine permit and adjacent area includes a mix of land uses. The lower elevation areas are <br />used for pasture,orchards, residential and industrial uses. Approval of Permit Revision No. 6 added hayland <br />to the list of permit area land uses. Agricultural uses are served by irrigation water. The higher elevations <br />within and adjacent to the permit area support some rangeland use, and the areas offer abundant wildlife <br />habitat. The lands also support various recreational uses. <br />Historic and current mining operations also exist in the general area. The Bowie No. 1 Mine is located west <br />of the Bowie No. 2 Mine permit area. The Terror Creek Loadout is located to the south of the Bowie No. <br />2 Mine permit area. The reclaimed new Blue Ribbon Mine is also located nearby along Hubbard Creek, as <br />are outlying facilities associated with the Sanborn Creek Mine. Historic coal mines located within and <br />adjacentto the Bowie No. 2permitboundary include the King Mine, the Gelwick Mine, the old Blue Ribbon <br />Mine and the Farmers' Mine. The old townsite of Bowie is located within the Bowie No. 2 permit area. <br />There are no known historical sites that are eligible to the National Register in the areas to be disturbed <br />under Permit Revision No. 6. Three historic sites, not associated with important persons or events in history <br />and not eligible to the National Register, were determined by the CHS to not have much integrity due to <br />deterioration and alteration. As requested by the Colorado Historical Society, BRL has committed to stop <br />construction and evaluate the situation appropriately, in consultation with the Colorado Historical Society, <br />if previously unknown cultural resources should be discovered. <br />Geology - <br />Detailed information regarding the geology in and adjacent to the Bowie No. 2 Mine permit area is provided <br />in Sections 2.04.5 and 2.04.6 of the permit application document. Abrief summary is provided below, and <br />this summary is derived from the information presented within Sections 2.04.5 and 2.04.6 of the permit <br />application. <br />The Bowie No. 2 Mine permit area is located in the North Fork Valley of the Gunnison River, near the <br />western margin of the Colorado portion of the Central Rocky Mountains. The elevation of the permit area <br />ranges from about 6,000 feet above sea level to over 8,000 feet above sea level. The general area is situated <br />along the southern flank of the Piceance Creek structural and sedimentary basin. The area is bounded by <br />Larimide structural and physiographic features on the following sides: West Elk and Elk Mountains on the <br />east; the Gunnison Uplift on the south; the Uncompahgre Uplift on the west-southwest; and the Grand <br />Mesa-Piceance Basin on the north. <br />The geologic structure of the eastern permit area exhibits an attitude of N70°W and dips 3 to 5 degrees to <br />the northeast. The western permit area exhibits an attitude of N88°W to N76°W and dips 4 to 7 degrees to <br />the northeast. The structural dip direction changes near Terror Creek due to faulting. There are numerous <br />faults located within and adjacent to the permit area. The faults in the central portion of the permit area are <br />high angle normal faults. These faults trend N40°W and dip 70 to 80 degrees to the northeast. The fauhs <br />have a strike -slip component. The throw of the faults ranges from 7 to 30 feet. <br />The coal in the area is situated within Mesaverde formation which contains interbedded sandstones, <br />mudstones, shales, siltstones and coal beds. The Mesaverde formation lies upon the Rollins Sandstone <br />14 <br />