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<br /> <br />Exhibit D <br />Mining Plan <br />The proposed mining activity will take place on the low bluffs <br />that rise above the valley floor south of the Arkansas River <br />down-stream from Canon City. Mining will begin in phases bef,in- <br />ning with the area presently permitted by the Colorado MLRf3 and <br />be completed in about 10 years on adjacent land to the west. The <br />mining activity will leave a neatly graded terrace overlooking <br />the Arkansas River valley that is ideally suited for home sites. <br />The gravel deposit found on the lower reaches of the bluff is <br />underlain by a layer of sandstone. The 'sandstone appears at the <br />surface level of the present mine floor along the northern bound- <br />ary of Area A, as shown on the map, Exhibit C. The sandstone <br />layer tilts downward at about a two degree angle on an east/west <br />axis so that at a distance of 450 to 500 ft, south, the layer is <br />found about 10 to 12 ft. below the elevation of the nearly level <br />mine floor. <br />The sandstone layer, tilced to the south, creates a natural. <br />groundwater reservoir beneath the bluffs that parallel the river. <br />No mining activity will disturb the groundwater reservoir. As <br />in the past, all mining will halt above the groundwater table. <br />In its natural state the gravel deposit is about 18 ft. thick <br />along the northern boundary of the proposed area and dips with <br />the sandstone layer into the bluff to the south. The over bur- <br />den ranges from near zero on the north to 40 ft. or more further <br />south, which is due in part from the natural rise in the terrain <br />on the proposed area. ConsegNently, as mining proceeds south <br />into the bluff, the self-imposed determination to mine above the <br />groundwater table reduces the amount of available gravel deposit. <br />