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The New Horizon Mine 1 produced coal from both the upper and lower Dakota coal <br />seams. The upper Dakota coal seam ranges in thickness from 1.6 feet to <br />3.3 feet and is separated from the lower Dakota seam by 7 to 11 feet of <br />interbedded sandstone and shale. The lower Dakota seam varies in thickness <br />from 5.9 feet to 7.9 feet. The base of the lower Dakota coal is 83 feet above <br />the top of the Burro Canyon Formation. The coal dips to to 20 southwest <br />and strikes N 25oW to N 45o W. <br />The New Horizon Mine 2 will primarily produce coal from the lower Dakota coal <br />seam and may utilize the upper Dakota coal seam during subsequent permit terms <br />if the seam is thick enough and of sufficient quality. The lower Dakota coal <br />seam at New Horizon Mine 2 ranges in thickness from 4.2 feet to 6.9 feet and <br />is 99 feet above the top of the Burro Canyon Formation. The coal dips <br />4.5o SW along a strike of N 45oW. <br />Surface Water <br />The San Miguel River has its source in the San Juan Mountains. These <br />mountains are primarily composed of Tertiary volcanic rocks. Iorns <br />et. al. (1965a) has shown these waters to be of a calcium bicarbonate - <br />sulfate type during high flow periods. These waters contain less bicarbonate <br />during low flows while the calcium and sulfate concentrations increase due to <br />less dilution from snowmelt runoff. The San Miguel River traverses the <br />interior portions of a basin that is chiefly underlain by Dakota Sandstones, <br />the Morrison Formation and Mancos Shales. The Morrison Formation and Mancos <br />Shale have the greatest potential for influencing the river water chemistry. <br />The San Miguel River drains an area of 1,080 square miles. In addition, <br />approximately 15,500 acres of irrigated land lies between Placerville and <br />Naturita, Colorado. It is estimated that 2.8 tons of Total Dissolved Solids <br />(7D5) per acre are contributed to the waters annually from this area. This <br />results in increased levels of magnesium, potassium, sulfate and chloride. <br />Water quality samples taken from the San Miguel River at Naturita, Colorado, <br />have a weighted average of 316 milligrams per liter (mg/1) TDS. Specific <br />conductance varies between 318 and 730 millimhos (mmhos). The mean sodium <br />adsorption ratio (SAR) is about 0.7 at Naturita. Water curves indicate that, <br />90 percent of the time, flow in this river exceeds 60 cubic feet per second <br />(cfs), while flows exceed 1000 cfs about 10 percent of the time. The mean <br />discharge of the river is 351 cfs. San Miguel River waters are suitable for <br />domestic usage except at low flow periods when sulfate levels are high. <br />The Colorado Cooperative Ditch Company diverts as much as 155 cfs of water <br />from the San Miguel River approximately ten miles east of the town of Nucla. <br />The main diversion ditch then flows westerly passing just north of the town of <br />Nucla and then flows northwestward passing north of the New Horizon Mine 1. <br />Diversion ditches distribute water to mainly agricultural users in the area. <br />Additional uses include domestic, municipal and stock pond consumption. <br />The New Horizon Mine 1 is located downslope from the main ditch in the gently <br />sloped upland of Second Park. This is just north of Tuttle Draw and is <br />totally within its watershed. The New Horizon Mine 2 site is just west of the <br />town of Nucla and is located in the mildly sloping upland area immediately <br />north of Calamity Draw, approximately in the middle of First Park. The <br />above-mentioned parks consist of recent undifferentiated aeolian silts and <br />sands overlaying the Dakota and Burro Canyon Formations. Since the completion <br />-5- <br />