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2008-08-11_PERMIT FILE - C1992080A
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2008-08-11_PERMIT FILE - C1992080A
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Last modified
8/24/2016 3:35:22 PM
Creation date
12/29/2009 8:44:20 AM
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Template:
DRMS Permit Index
Permit No
C1992080A
IBM Index Class Name
Permit File
Doc Date
8/11/2008
Doc Name
Revised Permit Document
Section_Exhibit Name
Abridged Permit Document
Media Type
D
Archive
Yes
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0 2 04 7 Hydrolou Description <br />2.04.7M Groundwater Information <br />Drilling information obtained to date does not indicate the occurrence of a widespread <br />water table associated with an unconfined aquifer. Three stratigraphic intervals have <br />been determined to hold and transport varying quantities of groundwater. One is a 1.3 <br />foot thick zone at the base of the Lewis coal zone in the north end of the proposed pit. <br />This zone is monitored by Well 17B where it is located 45.6 to 46.9 feet from the surface <br />(Map 4 -3). The second water bearing zone consists of a 96 foot thick interval extending <br />from the top of the Shamrock coal zone to the base of the Carbonera coal zone. This <br />zone was monitored by Well 82 -5 where it is located from 101.3 to 197.5 feet from the <br />surface (Map 4 -3). The third water bearing zone consists of a 17 foot thick zone adjacent <br />and above the Shamrock Rider Coal Zone. This water zone will be monitored by Well <br />82 -4 although its occurrence is outside the planned pit disturbance. The zone was <br />intercepted 383 to 400 feet below the surface in Hole 82 -4 (Map 4 -2, Surface Geology <br />Map). <br />The strata bearing these water zones dip 27 to 30 degrees to the southeast, extending <br />beyond the permit area and beyond the adjacent area. Lithologically these water bearing <br />zones occur in fractured strata and does not appear to be interconnected or contiguous. <br />Fractured shales appear to be the dominant source of water although limited water can <br />also occur in the coal seams. Vertical communication may also exist between certain <br />areas by faulting although no faults have been found in the current mining area. <br />Correlation of drill holes resulted in the identification of potential faulting or other <br />thickening and thinning of strata. <br />No seasonal variation of these waters have been observed. The monitor wells are not <br />pumped; consequently no changes in water quality has been observed. During the next <br />four quarters the three existing wells will be pumped and tested to more fully characterize <br />the groundwater. Prior to mining two additional holes will be drilled to test the depth and <br />quality of the coal seams. As these wells are drilled, the water encountered will be tested <br />for quality and quantity. This information will be added to the baseline information in <br />this permit. Well 82 -5 was destroyed as the mining progressed to the north and is no <br />longer available for any use in monitoring. <br />There are no known uses of the water in these three water bearing zones. Based on <br />current drilling information, there is no free water table. The permittee is the owner of <br />any and all groundwater resources by virtue of its surface ownership. <br />Groundwater quality analyses for the water samples taken from drill holes 17B and 82 -5 <br />are contained in Table 4 -2 in Exhibit H (appendix 2.04) as well as in the separate Annual <br />Hydrologic Reports submitted to the Division from 1995 -2006. <br />• <br />Abridged Permit Document 4 -11 Feb 2008 <br />
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