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Coal Ridge No. 1 Mine C1984065: MT7 <br />Section I - Mine History and the Environment <br />April 14, 2014 <br />The Coal Ridge No. 1 Mine is in permanent cessation. No coal production is planned for the current <br />permit term. Proposed activities include reclamation, maintenance, and monitoring activities. <br />The mine is located on private lands within Garfield County. The legal description of the lands <br />included within the permit area is: <br />Those lands in the NE % yet south of County Road 335, Lots 3 and 4, S %, S % NW %, Section 1, and the <br />N % NE % Section 12, Township 6 South Range 91 West 6th Principal Meridian; and the S % SW <br />Section 5, all lands south of County Road 335 Section 6, NE %, N % NW % Section 7, N %, N % SE %, NE <br />SW % Section 8, S % NW %, SW % Section 9, NW % Section 15, and N1/2 NE %, NE % NW Y4 Section <br />16 Township 6 South Range 90 West 6th Principal Meridian, Garfield County, Colorado. <br />These areas of the permit are covered by USGS 7.5- minute topographic maps Storm King Mountain <br />and New Castle quadrangles. The permit area is located to the south of the Colorado River, <br />approximately 7 miles west of Glenwood Springs, Colorado; and on the south side of County Road <br />335, approximately 1.5 mile east of the 1 -70 105 New Castle, Colorado interchange. The reclaimed <br />disturbed areas (the mine portal and facilities area) are located at the base of a steep escarpment of <br />the Grand Hogback. <br />Description of the Environment <br />The surface facilities of the mine were located on north - sloping fan terraces at the foot of the Grand <br />Hogback. The lower terraces of the site, at elevation approximately 5,800 feet, are approximately 150 <br />feet above the Colorado River, and are used as cropland (grass and alfalfa) and for grazing. The base <br />of the steep slopes is used for grazing (sagebrush areas). <br />Geology <br />Rock strata dip ranges from 30 to 70 degrees to the west - southwest. Minor folds trending north - <br />south to northwest - southeast occur throughout the region. However, there is little evidence of <br />faulting along the Grand Hogback. <br />The exposed rock sequence in the permit area is Jurassic through Tertiary in age and includes <br />(proceeding from the base to the top, oldest to youngest) the Morrison Formation, Dakota <br />Sandstone, Mancos Shale, the coal- bearing Mesaverde Group, and the Wasatch and Ohio Creek <br />formations. <br />The stratigraphy of the Mesaverde Group includes interbedded and lenticular sandstones, shale, <br />siltstone, and coal beds. In ascending order (oldest to youngest), the Group contains (1) the Corcoran <br />Sandstone, a marine shale sequence, and the Rollins Sandstone; (2) the Bowie (coal- bearing) <br />member; (3) the Paonia (coal- bearing) member; and (4) the Upper (non -coal bearing) member. The <br />Page 3 of 28 <br />