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Dowe Flats Quarry Site Description and Future Mining Impact Analysis <br /> 2.3 Areas Subject to Flooding <br /> After the 2013 flood, The Colorado Water Conservation Board re-mapped the 100-year flood <br /> zone. This boundary has been adopted by the Boulder County Commissioners for use in <br /> regulatory decisions and is available online from the Boulder County website (Boulder County <br /> 2020b). The Dowe Flats property is not within the 100-year flood zone. No activities proposed in <br /> the permit amendment application will occur within the 100-year flood zone. <br /> 2.4 Lakes <br /> There are no lakes within the Dowe Flats permit area. No activities proposed in the permit <br /> amendment application will impact any lakes. <br /> 2.5 High Ground Water Areas <br /> The primary source of ground water in the Dowe Flats permit area is an unconsolidated shallow <br /> alluvial aquifer of Quaternary age that ranges between 12 and 30 feet thick. The well yields in <br /> this aquifer are classified by the Colorado Geological Survey(CGS)as being small to inadequate <br /> (less than 15_gallons per minute) (Hall et al. 1980). The Niobrara Formation and Pierre Shale, <br /> both Cretaceous-age sediment formations, underlie the unconsolidated alluvium. These <br /> formations are both classified by the CGS as aquifers with inadequate well yields of less than <br /> one gallon per minute. Previous mining through these aquifers has yielded little to no production <br /> of groundwater into the mine pit.No activities proposed in the permit amendment application <br /> will have new impacts on groundwater quantity or quality. <br /> 2.6 Topography <br /> Dowe Flats is in a triangular-shaped valley that resulted from erosion of less-resistant geologic <br /> strata in the interior of a plunging syncline. Ridges of more resistant beds surround the valley on <br /> three sides. The Hi-Cal Ridge that runs down the western edge of the current mine area transects <br /> the western half of the larger valley. In general,the valley floor has low topographic relief and <br /> slopes toward the south at an average 2%gradient. The highest point on the Dowe Flats property <br /> at the north end of the Hi-Cal Ridge is approximately 5,470 in elevation and the lowest elevation <br /> at the south end of the property near Highway 66 is 5,240 feet. <br /> The Dowe Flats property currently has more topographic relief than it did before mining or than <br /> it will when mining is complete. At the south end of the Hi-Cal Ridge, there is a large <br /> overburden stockpile where the crusher facilities currently sit. There is another large overburden <br /> stockpile to the southeast of the Hi-Cal Ridge,referred to as Mt. George on the site plan map. <br /> There are also three pits in the current mining area and several growth media stockpiles around <br /> the outer edges of the property. Based on the current reclamation plan, the overburden and <br /> growth media stockpiles will be redistributed to fill in the mining pits and entire property will be <br /> graded to tie into the existing undisturbed topography and gently slope toward the south except <br /> for a 20-acre depression on the northeast side that will be developed into a wetland. <br /> 2.7 Current Land Use <br /> The property included in the permit area of this application currently operates as a permitted <br /> mine site. The types of activities occurring within the Dowe Flats property include: <br /> • Stripping <br /> Habitat Management, Inc. 3 May 2, 2022 <br />