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APPCOR10092
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APPCOR10092
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Last modified
8/24/2016 6:26:31 PM
Creation date
11/19/2007 2:07:46 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981033
IBM Index Class Name
Application Correspondence
Doc Date
7/16/1982
From
OSM
To
BEAR COAL CO INC
Media Type
D
Archive
No
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• FINDINGS <br />Bear Coal Company's <br />Application for Mining and Reclamation Plan <br />and Reclamation for Bear ~1, ~2 and ~3 mines <br />Upon review of the mining and reclamation plan submitted November 12, 1981 and <br />updated through March, 1982, I find that: <br />1. The plan and the permit application is accurate and complete and all <br />requirements of the Surface Mining Control and Reclamation Act (the "Act"), <br />the Colorado State Program, and the Federal Lands Program, including the Min- <br />eral Leasing Act, have been complied with (See Technical Analysis [TA] <br />[2.07.6(2)(a), 786.19(a)]. <br />2. The applicant has demonstrated that coal mining and reclamation <br />operations, as required by the Act, the Colorado State Program, and the <br />Federal Lands Program, can be feasibly accomplished under the mining and <br />reclamation operations plan contained in the application (see TA) <br />3. The assessment of the probable cumulative impacts of all anticipated <br />coal mining in the general area of the operations on the hydrologic balance <br />has been made by Office of Surface Mining and the Colorado Mined Lands Recla- <br />mation Division. The assessment included the Orchard Valley, Blue Ribbon, <br />• Somerset, Hawkes Nest, Mt. Gunnison and Bear mines. <br />The rejuvenation of the Old Edwards Mine into the Bear ~3 Mine will have an <br />insignificant effect on the probable hydrologic balance in the permit area re-_ <br />suiting in an almost nonexistent effect on the cumulative probable hydrologic <br />impact of all anticipated mining in the area. OSM reached this conclusion by <br />considering the following evidence: <br />a) Bear ~3 mine will mine in the upper Cretaceous, Mesaverde Formation, <br />Lower Coal Member "C" seam. This seam has a formidable sandstone bar- <br />rier above it that has a thickness of about 150 feet. This sandstone, <br />as evidenced by previous mining in the immediate area in the "C" seam, <br />acts as a hydrologic barrier for the "C" seam mines. Historically the <br />"C" seam mines that mine up dip have been unusually dry with water re- <br />quired for mining needing to be pumped in. Two examples of this dry- <br />ness are the Bear t~l mine and the old workings of the proposed Bear ~3 <br />Mine 1/4 mile downstream. Both are outcrop mines on the same site of <br />the river channel and mined in the "C" seam. Both are exceptionally <br />dry even in the areas where pillar supports were pulled and roof <br />cracking could be expected to occur. The only water that has been <br />encountered is occasional occurrences of "fossil" or "insite" water in <br />the coal released by mining and quickly dries up. The "C seam" is not <br />considered to be an aquifer. <br />b) The "C" seam outcrop at the proposed Bear ~3 Mine is in the cliff area <br />about 140 ft above the North Fork stream channel (stream is immediate- <br />ly north of the mine area) and the "C" seam has a stratigraphic dip <br />• that ranges from 3-5 degrees to the north-northeast. The existing <br />portals of the proposed Bear ~3 Mine (the old Edwards Mine portals) <br />
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