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2011-01-13_PERMIT FILE - C1981038A (3)
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2011-01-13_PERMIT FILE - C1981038A (3)
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Last modified
8/24/2016 4:28:56 PM
Creation date
4/6/2011 10:30:38 AM
Metadata
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Template:
DRMS Permit Index
Permit No
C1981038A
IBM Index Class Name
Permit File
Doc Date
1/13/2011
Section_Exhibit Name
Groundwater Appendix
Media Type
D
Archive
Yes
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• Ground water from the shallow colluvial/alluvial aquifer in <br />the Stevens Gulch drainage is used by Colorado Westmoreland, Inc. <br />for water supply. <br />A more detailed discussion of ground water hydrology in the <br />permit area is included in the existing approved mine permit <br />and Brooks, (1983). <br />3.2 Site Hydrogealogy <br />The ground water in the drainage basin of East Roatcap Creek <br />where the proposed new portal bench is located occurs in <br />colluvial sediments and in the bedrock of the Mesaverde <br />Formation. <br />3.2.1 Data Aquisition <br />The local ground water characteristics were obtained in <br />several phases of investigation. In 1977 the U.S.G.S. installed <br />a monitoring well (GR-77-7) in the central part of the East <br />Roatcap Creek drainage. This well is screened in the sandstone <br />strata of the Mesaverde Formation. The depth to water level in <br />this well fluctuates at approximately 115 feet below the ground <br />surface. <br />In 1982 two deep exploration wells, DH-60 and DH-65 were <br />~~~ equipped for ground water monitoring. Both of these wells are <br />open in the coal bearing member of the Mesaverde Formation. <br />In July, 1985 three shallow monitoring wells, SM-5, SM-6, <br />and SM-7 were installed in the colluvial sediments within the <br />East Roatcap Creek drainage basin. All three of these wells were <br />used for permeability testing and for collection of water quality <br />samples. <br />In July, 1986 three additional monitoring wells, SM-10, SM- <br />11 and SM-12 and eleven piezometers (DH-81, B1S, 82C, 825, 83C, <br />83S, 84C, SSC, 86, 87, and 885) were installed near the proposed <br />portal bench area. Afield permeability test was performed in <br />five of these monitoring wells and piezometers. At this time a <br />total of 13 shallow monitoring wells (colluvium) and 7 deep <br />(bedrock) monitoring wells are available within the East Roatcap <br />Creek drainage basin. The location of the monitoring wells are <br />shown on Figures H-4 and H-5 and on Drawing DO1 SO118 in the <br />confidential volume of the approved permit to mine. Construction <br />characteristics are shown in Table H-3 and on Figures H-6A and H- <br />6B. <br />During 1982 and 1983 an intensive reconnaissance study of <br />ponds, springs and seeps within the East Roatcap Creek drainage <br />• ~ basin was performed. From a total of 28 ponds and 4 springs, 6 <br />ponds and 1 spring were selected for monitoring. All of the <br />identified springs are issuing water from the colluvial <br />sediments. <br />
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