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Finally, some considerations in planning on mining in the vicinity of the Idaho No. 1 and the <br />May Day No. 1 mine has been considered. This preliminary analysis suggests that the <br />primary saturated flow occurs along faults and fractures that are predominately east west <br />trending and north -south trending veins. The planned operations will be in the May Day No. <br />1 tunnel area. This area is topographically higher than the potential discharge points located <br />in the vicinity of the Idaho No. 1 mine and at least until other data becomes available, <br />saturated flow along the faults and the fractures should be assumed to travel with topography. <br />7.0 REFERENCES <br />recommendation 1 and continue that analysis. Should this information suggest <br />increased flow, examine the potential source areas for geologic characteristics and <br />area. From this information, a potential recharge volume can be suggested for the <br />mine area. <br />Carlson, Mike, 2003. Practical Reservoir Simulation. PennWell Corporation, Tulsa, Oklahoma. <br />575 pp. <br />Christensen, O. D., 2007. May Day Idaho Mine, La Plata County, Colorado. Prepared for <br />Wildcat Mining Corporation. <br />Eckel, E.B. 1949. Geology and Ore Deposits of the La Plata District Colorado. U.S. Geological <br />Survey Professional Paper 219. <br />Freeze, R.A. and J. A. Cherry. 1979. Groundwater. Prentice -Hall, Upper Saddle River, New <br />Jersey, 604 pp. <br />Gloyn, R.W., C. D. Morgan, D. B. Talbot, R.E. Blacken, B. T. Tripp, Mike Lowe; 1995. <br />Mineral, Energy and Ground -water Resources of San Juan County, Utah. Utah Geological <br />Survey, Utah Department of Natural Resources, Special Study 86.39 pp. <br />Linsley, Ray, K. and Joseph B. Franzini. 1972. Water - Resources Engineering. McGraw -Hill, <br />Inc. New York. 690 pp. <br />Robinson, G.M.L.R. 2011. Personal Communication. <br />