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Cross -Mountain Ranch, LLC owns property within the Permit Area that will be affected by mining of Panels 13 - <br />through 17 -Left, and Fish Creek and its associated AVF will be affected within their property boundaries by <br />mining of Panels 14- through 16 -Left (T5N, R87W, Sections 19, 24, and 25). As presented in Exhibit 25Z, a <br />• total of 39.9 acres will be flooded under normal flow conditions by mining of these panels. As is the case for all <br />the lands along Fish Creek to be undermined and subsided, no flood irrigation system has been established to <br />increase the productivity of the land, nor are management practices established for haying this area. The land is <br />treated as unimproved rangeland utilized for grazing by the lessee. <br />TCC's mining and subsiding of Fish Creek and its associated AVF will not impact those AVF's located <br />downstream of the operation. Subsidence of the valley floor above Panels 17- and 18 -Right and Panels 13 - <br />through 16 -Left will result in the formation of pools, with pooling and flow conditions similar to those experienced <br />in those areas overlying Panels 9 -Right in the EMD and Panels 13- through 16 -Right in the NMD. <br />It is anticipated that the Fish Creek channel will respond in the same manner as the Foidel Creek channel (see <br />PR03) for the entire length where it crosses Panels 17- and 18 -Right and Panels 13- through 16 -Left. The entire <br />length of Fish Creek overlying these panels was surveyed to identify any outcrop areas. The survey showed that <br />a rock outcrop (Fish Creek Sandstone) was exposed in approximately 1,260 feet of channel in Section 10, T5N, <br />R86W. Surficial cracking could occur in this area, and it would be a potential site for bedrock recharge. The <br />cover is greater over these panels, however,and has additional shale between the mined intervals and the surface. <br />This shale is the unit over which the alluvial materials were deposited. The combination of greater depth and <br />thicker shale deposits will minimize the potential for surficial cracking and surface water communication to <br />occur during and after mining. Given these considerations, TCC does not anticipate any significant loss of flow <br />in Fish Creek as a result of its mining operations. <br />If one were to look at the worst-case of flow disruption in Fish Creek, it would be prudent to assume that the <br />same loss as experienced in Foidel Creek would occur. Also, it should be understood that the loss would be <br />experienced over each of the panels and not all at once, thus limiting the volume of water that would enter the <br />• bedrock system. As presently shown on Map 23, mining will progress from the south to the north in the NMD. <br />Panel 17 -Right is the first panel in this part of the NMD that will result in subsidence potentially impacting Fish <br />Creek and its AVF. Fish Creek meanders over the panel for approximately 2,300 feet. Using the above - <br />referenced relationship of stream length to recharge volume, results in approximately 14 ac -ft of water <br />potentially recharging the bedrock. In reference to Panel 18 -Right, Fish Creek meanders over the panel for <br />approximately 1,700 feet. This will result in approximately 10 ac -ft of water potentially recharging the bedrock. <br />Given the volume of water that passes through the Fish Creek system, any loss during the year is not significant <br />to the irrigation systems on lower Fish or Trout Creeks. <br />Table 72 B, NMD Recharge Time Estimate, provides the number of days it would take to fill in the additional <br />fracture volume resulting from subsiding the bedrock. Again, it should be recognized that this is a very <br />conservative estimate, due to the character of the stream. The data presented assumes that sandstone bedrock <br />can be found for the entire length of Fish Creek overlying the panels, and this is not the case. The section in <br />which the sandstone unit is exposed is the approximate 1,260 feet of channel in Section 10, T5N, R86W. The <br />remainder of the channel is alluvial material overlying the Lewis Shale. Given the nature of the shale, it will <br />swell to fill in any cracks that may occur. <br />TCC is the immediate downstream user of irrigation water, and does not foresee any impacts to its agricultural <br />operations due to the potential loss of water from the system. In the event that significant losses occurred <br />during the irrigation season, TCC has sufficient water rights under the approved Augmentation Plan to augment <br />any loss. In reference to water quality impacts, the ongoing downstream monitoring at Station 900 on Foidel <br />Creek does not show any changes that can be attributed to subsidence over Panels 8- and 9 -Right. Refer to <br />TCC's recent Annual Hydrology Reports to review this data. <br />• In order to validate that no impacts will be realized to the AVF downstream of its operations, TCC will <br />continue to monitor downstream surface and alluvial water monitoring stations. These stations are presented on <br />Map 13A, Hydrologic Monitoring Program. The stations will be monitored consistent with the existing <br />PR09-08 2.06-25.6 09/29/09 <br />