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2010-03-15_PERMIT FILE - C1981035A (6)
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2010-03-15_PERMIT FILE - C1981035A (6)
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Last modified
10/20/2016 7:32:14 AM
Creation date
6/16/2010 2:19:07 PM
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Template:
DRMS Permit Index
Permit No
C1981035A
IBM Index Class Name
Permit File
Doc Date
3/15/2010
Doc Name
HYDROLOGY DESCRIPTION
Section_Exhibit Name
KII 2.04.7 Hydrology Description
Media Type
D
Archive
Yes
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connection between the King II Mine and the Cliff House sandstone in <br />• their location. Therefore, no potential for impacts exists. <br />Menefee Formation <br />The upper part of this formation contains the coal seam to be mined at <br />the King II Mine. Sixty seven years of mining at the King I Mine two <br />miles southeast has not encountered any ground water in this formation. <br />Well Number 1, which is drilled in and draws water from the Quaternary <br />alluvium, has a static water level 76 feet below ground level. Ground <br />level at that point is at an elevation of 7,390 feet above sea level. The <br />coal seam being mined is at an elevation of 7,450 feet. Thus, the mine <br />will be located at least 136 feet above the potentiometric level. There is <br />no indication that the aquifer will be affected by the King I Mine. <br />An exploratory core drill hole located in the SE /4 NW /4 of Section 32 <br />was driven from the surface through all the overburden strata to the <br />base of the currently mined upper Menefee coal seam at the King I Mine. <br />No water was encountered. A well core hole was driven in 1978 on the <br />King I Mine bench near the water tank to a depth of ninety feet. The well <br />was dry. The collar of the well is below the upper Menefee seam outcrop. <br />These two holes along with the previously mentioned active water wells <br />indicate that the overburden strata, and strata at least to a depth of <br />twenty feet below the lower Menefee coal seam contain no aquifers. <br />The best evidence is, however, of no disturbed aquifers or no aquifers <br />and no ground water seepage in the mine workings themselves, except <br />for local perched aquifers. Water must be pumped into the King I Mine <br />from Wells # 1 and # 2 for dust and fire control. This is a normal need <br />for operating coal mines. Intake water used inside a mine is typically not <br />pumped out or discharged. <br />Point Lookout Sandstone <br />The Point Lookout Sandstone is below the formation to be mined and will <br />not be disturbed during the mining process. The upper 100 to 140 feet <br />is massive sandstone which may or may not contain significant amounts <br />of ground water. Wells have recently been drilled into this unit for new <br />real estate developments (Rafter J.) approximately ten miles east of the <br />project area. Small amounts (max. pump rate of 30 gpm) of water were <br />encountered in some locations. <br />Searches of the records of the Colorado Division of Water Resources for <br />the King I Mine and personal observations of Fred M. Johnson, Certified <br />Professional Geologist, indicate that quality of water in the massive <br />• vc.. �i. �siririwi® rsisiairisirroirrrior® irimsr® r® r® r® rsi�rrsisisrsraorirr® ierisisiwror�r® isrwiiui® ioisirivirisi® iwie�rrr irrs ®i ®rsrii ®is ®isurrr. <br />GCC Energy, LLC King II Mine <br />Section 2.04.7 <br />Page 2 October, 2008 <br />7 / S- <br />
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