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2014-05-20_REVISION - C1982056
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2014-05-20_REVISION - C1982056
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Entry Properties
Last modified
8/24/2016 5:44:08 PM
Creation date
5/21/2014 7:25:46 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1982056
IBM Index Class Name
Revision
Doc Date
5/20/2014
Doc Name
Adequacy Responses
From
Twentymile Coal, Inc
To
DRMS
Type & Sequence
TR83
Email Name
JDM
DIH
Media Type
D
Archive
No
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With the additional geologic information obtained from the ongoing drilling, Map 23d has been <br />updated to show the Wolf Creek interburden thickness. <br />➢ All drilling to date has not encountered any significant groundwater below the Wadge Coal <br />Seam, as evidence by the lack of increases in return flows during the drilling operations. <br />➢ The lithologic sequence does not include any significant clay layers immediately above or <br />immediately below the Wolf Creek Coal Seam. <br />2. Per Rule 2.04.7(1)(a)(i), (ii), (iii), (v), and Rule 2.04.7(b) no discussion concerning the any <br />aquifers related to the Wadge /Wolf Creek interburden, the Wolf Creek coal seam, or, if potentially <br />impacted, strata directly below the Wolf Creek coal seam has been provided. The Division has <br />studied the Williams Fork Formation here and at other nearby mines and has made findings in the <br />past regarding the need for baseline groundwater information below the Wolf Creek Coal which is the <br />lowest coal seam to be mined with this proposed mine plan area. The Division has determined that <br />there is no potential to impact the Trout Creek Sandstone which is the significant aquifer that <br />underlies the Wolf Creek Coal. The Trout Creek Sandstone is a confined aquifer under potentiometric <br />head. The confining shale layers above the Trout Creek Sandstone should prevent any integration of <br />water from the overlying Wolf Creek Coal seam. The Foidel Creek PAP also discusses the hydraulic <br />isolation of the Trout Creek Sandstone. Additional baseline data collection will be necessary to <br />identify potential groundwater impacts below the Wadge Coal Seam and within the Wolf Creek <br />Coal seam. Characterization of the quantity and quality of water within each aquifer /saturated <br />zone above and within the Wolf Creek Seam is required. Please provide a plan for review that <br />addresses baseline characterization of the Wadge CoaUWolf Creek Coal Interburden and the <br />Wolf Creek Coal Seam. The plan, description, and associated maps should include both up <br />gradient and down gradient monitoring wells and the Hydrologic Monitoring Plan and Probable <br />Hydrologic Consequences portions of the permit document updated accordingly. <br />Response: TC has worked closely with the Division to identify and develop reasonable baseline <br />hydrologic information to adequately characterize the groundwater hydrologic system. Plans and <br />relevant information have been incorporated in the expanded description of baseline surface and <br />groundwater conditions in Sections 2.04.5 and 2.04.7, and the revised PHC discussion in Section <br />2.05.6(3) of the PAP which accompany these responses. <br />In framing the hydrologic baseline and impact discussions, the following considerations are important <br />(as further detailed in the referenced PAP discussions): <br />➢ The Wolf Creek Reserve area underlies areas of the Wadge Coal Seam which have been <br />previously mined, consequently, any mining - related impacts on the Wadge Seam and <br />associated overburden units have already occurred, as characterized and discussed in the <br />current relevant PAP sections. <br />Exploration drilling of the Wolf Creek Seam and associated units (Wadge /Wolf Creek <br />Interburden, and immediate underlying units) has not encountered any significant amounts of <br />groundwater, as evidenced by the lack of any significant increase in normal return flows during <br />drilling operations. <br />As noted in the Division's comments, the potential for the plamied development and future <br />mining activities in the Wolf Creek Seam to impact the Trout Creek Sandstone, as an important <br />regional aquifer, are negligible, given the distance of the Trout Creek Sandstone below the <br />
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