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Exhibit G Water Information (cont) <br /> influence the groundwater levels and impact the baseline range <br /> and trigger point . The natural groundwater depths vary from 3 . 5 <br /> to 8 . 8 feet below the surface in Phases 1 and 2 when they were <br /> measured in March-2019 . The seasonal operation of the unlined <br /> irrigation return flow ditch that crosses the permit area on the <br /> west will affect groundwater levels and could help with any <br /> mitigation needs in the Phases west of the highway. Between the <br /> Platteville Ditch and the Railroad in Phases 4 , 5 , & 6 , the <br /> groundwater depth varies from 3 to 24 feet below the surface, <br /> when measured in March-2019 . Groundwater depths can vary <br /> significantly through seasons and years, depending on many <br /> influences, including, climate, precipitation, irrigation, other <br /> pumping rights, and much more . <br /> L .G. Everist, Ines . experience on other mines in the South <br /> Platte River valley indicates that groundwater levels can <br /> fluctuate as much as 7+ feet depending on the season. In a <br /> normal mitigation trigger plan, the trigger limits would be set <br /> at 3 foot change plus or minus change over a 3-month average . <br /> Realistically, in this case the trigger number should be based on <br /> a 3-foot change determined by a line that approximates a up or <br /> downward trend of the water table and considers outside impacts <br /> such as, drought , adjoining mining activities, storm events or <br /> decreased irrigation activities . At the current time, there is <br /> no mounding mitigation plan for when the water table increases . <br /> We do not expect this to be a problem where the slurry walls are <br /> in close proximity to a flowing water body like the ditches, <br /> return flow ditch and the South Platte River. Mounding would be <br /> controlled by those water surfaces and it would only affect <br /> Cannon Land Company areas around the reservoirs . On the east <br /> side of the Platte Valley Canal , the ground-water table averages <br /> 11 feet deep and there are enough unlined areas crossing thru the <br /> lined reservoirs to allow for some increase without impacting <br /> surface features . In the eastern area groundwater averages 12 <br /> feet below the surface, there are numerous, gaslines and road <br /> corridors that would allow ground water to bypass the lined <br /> areas . <br /> The mining operation will have minimal effect on the South <br /> Platte River in the form of minor groundwater depletions due to <br /> evaporation and water uses associated with mining. The depletions <br /> to the South Platte will be mitigated thru a temporary Substitute <br /> Water Supply Plan (as required and approved by the Division of <br /> Water Resources) to prevent injury to the vested senior water <br /> rights . <br /> The reclamation plan proposes the creation of 8 (or fewer) <br /> slurry wall lined reservoirs that will not be hydraulically <br /> L G. Evenst,Inc Ragsdale Reservoirs May 5,2020 <br /> 28 <br />