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PERMFILE59238
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PERMFILE59238
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Entry Properties
Last modified
8/24/2016 11:01:32 PM
Creation date
11/20/2007 6:11:46 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981038A
IBM Index Class Name
Permit File
Doc Date
6/29/2004
Section_Exhibit Name
2.05 Operation and Reclamation Part 3
Media Type
D
Archive
Yes
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52.05 APPLICATION FOR PERMIT FOR SIIRFACE OR UNDERGROUND MINING ACTLoITIES -- <br />MINIMUM REQUIREMENTS FOR OPERATION AND RECLAMATION PLANS. <br />2.05.6 Mitigation of Surface Coal Mining Operation Impacts. (Cont'd.) <br />(3) (b) (i) (Cont'd.) <br />~I <br />C~ <br />diverted directly to sedimentation pond num- <br />bers 3 and 4, now first pass through the waste <br />disposal area pond. <br />The fifth and final element in the Mine Site <br />Drainage Control Plan is the timber stocage <br />area sedimentation pond. All runoff drainage <br />from the timber storage area to [he south is <br />directed to the sedimentation pond (see Map <br />8-2). See Section 2.05.3(3)(b) for details on <br />the pond. Side slopes and top of area were <br />revegetated during the Fall, 1979. The areas <br />to the north have berms along the edge to di- <br />rect run-off from the [op to the road and fi- <br />nally into the sedimentation pond. These side <br />slopes were revegetated during [he Fall, 1979. <br />See Section 2.05.4(2). A vegetative buffer <br />below the side slopes was picked instead of a <br />sedimentation pond due to an increase in dis- <br />turbed area of approximately one acre that <br />would be required for a pond. The area is <br />small, approximately 0.5 acre. This run-off <br />would also go through oak brush vegetation be- <br />fore entering Steven's Gulch. See the Surface <br />Drainage Appendix - Vegetative Buffers in Vol- <br />ume 8. <br />Groundwater inflow into the Orchard Valley <br />Aline is very limited. During the year 1983, <br />only approximately 300,000 gallons of water <br />flowed inCO the mine. The source of Che <br />groundwater inflow into the mine is Che <br />perched water bearing sandstone above the <br />mined coal seam. This sandstone is of lentic- <br />ular character and the water bearing strata <br />are present only in parts of the permit area. <br />Groundwater inflow into the mine typically oc- <br />curs from fractures in [he roof strata. Some <br />water inflow was connected to the Fault en- <br />countered at crosscut /k77 in the North Mains. <br />In the 8 North Suhmain, damp ribs and floor <br />Added 12/26/84 <br />Revised IZ/26/84 <br />Revised 10(12/86 <br />Revised 10/01/87 <br />105 <br />
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