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RULE 2 PERMITS <br />Groundwater Uses <br />General Area <br />Groundwater uses in the general and permit areas of the Colowyo mine are minimal and of low volume. <br />Questions were raised in the past concerning well yields within four miles of the mine site. At that time <br />the Colowyo Coal Company undertook a program to investigate reported yields based on the Colorado <br />State Engineer's records. <br />A search of the State's files revealed that only three wells within four miles of the mine site have reported <br />well yields of 50 gal./min. The remaining wells have reported yields of less than 16 gal./min; most of the <br />wells have reported yields of less then 7 gal./min. The well yields were not field checked to determine <br />actual use or rate of use. There are no wells that have reported yields in excess of 50 gal./min. <br />Very little groundwater resource development has taken place in the Axial area. There are a few relatively <br />shallow, low-yield wells on or near the leasehold area that were dug for domestic purposes. <br />Permit Area <br />Groundwater uses in the mine area are also limited due to the depth to water and its limited overall <br />availability. Colowyo has developed two wells on the mine area to supply a portion of the domestic <br />needs. The two deep wells, Taylor Creek Nos. 1 and 3 are located in Section 33, T4N, R93W, and in <br />Section 4, T3N, R93W respectively. Taylor Creek No. 1, completed to a depth of 825 feet in the Williams <br />Fork Formation, produces 40 gpm with a static water level of 110 feet. Taylor Creek No. 3, completed to <br />a depth of 2,284 feet in the Iles Formation, produces 20 gpm with a static water level of 135 feet. <br />The information collected from the Colowyo Mine area indicates that groundwater is very limited, even to <br />depths significantly below mining activities. This conclusion is supported by the depths of the potable <br />wells, Taylor Creek No. 1 and Taylor Creek No. 3, necessary for sustained production. Further evidence <br />of lack of significant groundwater resources in and adjacent to the mine area is that residents in the <br />general area haul drinking water from Craig or Meeker. <br />Groundwater is not currently planned for industrial purposes such as watering haul roads or dust control <br />in the loadout facilities. Water for these purposes will be supplied by Wilson Reservoir located in Section <br />13, T4N, R93W. See Map 32 for the location of the reservoir and pipeline for conveyance to the mine <br />area. <br />Summary of Groundwater Conditions <br />The coal beds of the Williams Fork Formation that are to be mined are at a high elevation and are <br />truncated by the mining operation to the north, Goodspring Creek to the east and Taylor Creek to the <br />west. As a result, the coals and upper sandstones are drained. Perched aquifers exist in the coals and <br />sandstones, but exhibit little lateral or vertical continuity. Cascading waters from perched zones were <br />encountered during drilling of exploration holes on the lease. No substantial quantities of water were <br />encountered through the mine section or in the sandstones below the coals that are to be mined. <br />The Trout Creek Sandstone of the Iles Formation is the first major, regional aquifer that can be <br />recognized on the mine property. The sandstone occurs approximately 800 feet beneath the lowest coals <br />to be surface mined. <br />Rule 2 Permits 2.04.7-11 Revision Date: 6/23/08 <br />Revision No.: MR-91