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<br />i <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br />I <br /> <br />I <br /> <br />INVESTIGATIONS OF GROUND-WATER SUPPLIES <br /> <br />FOR PROPOSED MORGAN COUNTY <br />QUALITY WATER DISTRICT <br /> <br />Introduction <br /> <br />The following report is the result of investigations performed on <br /> <br /> <br />behalf of the Morgan County Quality Water Association. The investigations <br /> <br /> <br />were conducted during the summer and fall of 1973 for the purpose of eval- <br /> <br /> <br />uating certain ground-water reSOLrces for use as domestic water supplies <br /> <br /> <br />for a proposed water district in Morgan County, Colorado. <br /> <br />Three ground-water aquifers were considered. These are the alluvial <br /> <br /> <br />deposits of Lost Creek, Hay Gulch and Camp Creek, all of which are south- <br /> <br /> <br />side tributaries of the South Platte River. Figure 1 shows the location <br /> <br /> <br />of the areas investigated in relationship to Morgan County. <br /> <br />The scope of this report is limited to the geologic, hydrologic and <br />water quality aspects of the ground-water resources of the three aquifers. <br />Advice from legal counsel s]~uld be sought concerning the legal aspects of <br />developing and transporting the ground water to Morgan County for domestic <br />and livestock purposes. <br /> <br />Pertinent Considerations <br /> <br />The financial feasibility of constructing the pipelines, pumping plants <br />and storage facilities, such as are being planned for Morgan County, is <br />largely dependent upon having a reliable water supply. The reliability <br />must not ~nly be in the physical supply, but also in the legal rights to <br />the water. Equally important is the dependability of the quality of the <br /> <br />water. <br /> <br />Reliability of supply <br /> <br /> <br />The alluvial aquifers discussed in this report consist of unconsoli- <br /> <br /> <br />dated sand and gravel deposits lying in ancestral channels which were eroded <br /> <br /> <br />into the underlying bedrock materials. These deposits contain water, <br /> <br /> <br />derived from precipitation, which is slowly moving down slope towards the <br /> <br /> <br />South Platte River. Before man's influence on these systems, an equilibrium <br /> <br />M. W. BITTINGER AND ASSOCIATES, INC. <br />