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2015-08-18_PERMIT FILE - C1982056A (4)
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2015-08-18_PERMIT FILE - C1982056A (4)
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Last modified
8/24/2016 6:10:00 PM
Creation date
8/19/2015 1:06:42 PM
Metadata
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Template:
DRMS Permit Index
Permit No
C1982056A
IBM Index Class Name
Permit File
Doc Date
8/18/2015
Section_Exhibit Name
2.04 Environmental Resources
Media Type
D
Archive
Yes
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EMD and Southern Portion of WCR (ENID Panels 2 -Right through 9- Right, PR97 -04, TR13 -83) <br />The geology for the EMD is the same as that presented in Permit Revision No. 93 -03. However, Table 6B, 1997 <br />PR 97 -04 Federal Reserve Calculations for the Eastern and Northern Mining Districts, which is considered to be <br />confidential, presents the federal reserves that will be mined in the remainder of the Eastern Mining District and the <br />Northern Mining District. The detailed Wadge Seam structure is shown on Map 6, Wadge Seam Structures. The <br />geochemical data presented for PR 93 -03 is used for this revision as well. Geologic and geochemical data for the <br />Wolf Creek Seam are provided in Exhibit 53, Wolf Creek Reserve Geologic and Mine Plan Information. <br />The general geology and hydrology of the EMD has been described in previous permitting actions, i.e. original <br />application and updated with PR -3. During 1997, a drilling program was conducted to further define the geologic <br />setting in the remainder of the EMD. During this program particular attention was given to defining the Wadge <br />Seam parting that defines the southern limit of the EMD. Drillholes 97 -001 and 97 -003 were used to define the <br />southern mining limit. Both of these holes showed an in -seam parting of 1.9 - 2.5 feet and thinning of the seam. <br />The overlying stratigraphy is the same as previously discussed. This information was used to finalize the mine plan <br />as presented on Map 23. <br />Drill Site 97 -011, which was designed for multiple holes, was used to provide a better understanding of the fault as <br />it occurs in the Northeast sub - mains. Three borings were advanced at this location to determine the location and <br />magnitude of the fault. This was done by advancing two borings on the east side of the fault, with each boring <br />intersecting the fault. Another boring was advanced on the west side of the fault into and through the coal seam. A <br />deviation log was run in each of the holes to allow for accurate placement of end -point of boring. This data, along <br />with the other geophysical information, was used to correlate depth and seam thickness between each boring. After <br />the data was processed, the TCC Geologist was able to provide a better definition of the fault through the sub - <br />mains, which was then used to prepare a cut sequence through this area. <br />The expansion of the mine into the remainder of the EMD resulted in continued development of the Wadge Seam <br />reserves located in the Twentymile Park Basin. As discussed previously, this is an enclosed ground water basin <br />which is rimmed by outcrops of the major lithologic units. The units within this area include the Fish Creek <br />Sandstone (a local sandstone unit), Twentymile Sandstone, Marine shale, Wadge overburden (which includes the <br />Wadge seam),Wadge /Wolf Creek Interburden, Wolf Creek Seam, Wolf Creek Underburden, and the Trout Creek <br />Sandstone (which is a marker bed for TC). TC has not seen any deviation in the vertical orientation of these units <br />over the entire property, except for localized displacements caused by faults. <br />As indicated, the Foidel Creek Mine operates within a closed ground water basin. TC has completed monitoring <br />wells in the following formations within this basin: Twentymile Sandstone, Wadge Overburden, Wolf Creek <br />Interburden/Coal unit, Trout Creek Sandstone, and alluvial wells in the alluvium of Foidel, Fish, Middle, and Trout <br />creeks. The hydrologic gradients for all units are oriented towards the center (axis) of the basin. The EMD was <br />mined from south to north toward the center of the basin and immediately east of the major faults. As TC continues <br />mining, the focus of the hydrologic monitoring program will be on the Twentymile and Trout Creek Sandstones. <br />The EMD fault was first encountered in the 10 -Right gate -road and had a displacement of 22 to 23 feet, in the 9 <br />right gate -road the fault had a displacement of 13 to 15.5 feet, in the 8 -Right gate -road the fault had a displacement <br />of 8 to 15 feet, in the 7 -Right gate -road the fault had a displacement of 8 to 10 feet and in the 6 Right gate -road the <br />fault had a displacement of 13 feet. The faults were relatively dry when encountered and did not yield significant <br />flows to the mine, as documented by the Annual Inflow reports filed with the CDRMS. <br />TC mined through the fault and the steep grade zone in the 9 -Right and 8 -Right longwall panels. Given very <br />difficult mining conditions in this area, TC made the decision to modify the mine plans to avoid mining through the <br />fault and up the steep grade in longwall panels 7 -Right through 2 -Right <br />During the development of the 6 -Right gate -road, inflows were encountered from the Wadge Overburden between <br />crosscuts 24 to 27. The initial inflow was measured at approximately 265 to 275 gallons per minute. Maximum <br />TR13 -83 2.04 -16.1 11/03/14 <br />
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