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Exhibit C CMLRB 112 Permil Application <br />Agile Stone Systems, Inc. <br />• 2.0 COnC~US10I1S <br />1) Crossing designs were readily completed by a certified Colorado professional <br />engineer. Likewise storm water berms and ponds and other storm related <br />structures as well as other structures were all engineered by certified Colorado <br />professional engineer. <br />2) "The impact of the Project will be to increase the water table elevation beneath <br />the plant azea. This may also be reflected in the Dakota Group underlying the <br />plant area, with its water table or potentiometric head increasing somewhat (2 to 5 <br />feet), with lesser rises away from the plant. Slightly greater spring and seep flows <br />may also result." Gilmer <br />3) "The increased water table elevation would be more than offset by removing <br />irrigation from the hayfields and pastures of the adjacent ranch. This change <br />would occur at the direction of the Division of Water Resources, as the result of <br />its administration of junior water rights. This may lower the water table <br />sufficiently to reduce spring flows at the river and adversely affect downgradient <br />springs or wells." Gilmer <br />4) "The possible increases in potentiometric head or water table in the Dakota Group <br />could be manifested as somewhat greater bedrock spring discharge rates to the <br />Arkansas River, if DWR does not administer the junior irrigation rights. If <br />• irrigation is stopped, a decline in bedrock spring flows may occur." Gilmer <br />5) "Hydraulic impacts to the Dakota Group and other bedrock aquifers are not <br />expected to occur south of the Arkansas River, as the Arkansas River serves as a <br />hydraulic boundary having nearly constant-head conditions. Furthermore, faults <br />to the southwest, south, southeast and east of the project create structural blocks <br />that will be hydraulically sepazate bedrock units." Gilmer <br />6) Changes in bedrock well production or water quality (including hydrogen sulfide <br />presence) in the areas south of the River, and in wells producing water from <br />bedrock aquifers structurally isolated from the Project, will be due to natural or <br />other non-Project related factors." Gilmer Gilmer elsewhere noted that "No <br />bedrock water will be involved in the Pazkdale Project." <br />7) The project will not have any impact on either the Tallahassee Creek or Arkansas <br />River water flows or quality. Already purchased water rights will supplement any <br />water lost due to evaporation. Water percolating through the grave] from the <br />project will only contain sand or gravel sized material. The gravel bar will filter <br />any possible sediment long before the water reaches the Arkansas River exactly <br />like the sediment is filtered from the Tallahassee/Currant Creek waters passing <br />under the gravel baz or used in flood irrigation above the Steer's spring. <br />4 <br />