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Rimrock Mine Well Analysis <br />General Information <br />Greg Lewicki and Associates vvas asked by Mark Kerr of Landmark Reclamation, Inc. <br />to review all historical well data and groundwater information to see if groundwater <br />monitoring could be terminated at the Rimrock Mine near Trinidad, Colorado. <br />Considerable data is available for the three wells currently sampled: 1) the Montoya <br />dug well, located downstream of the permit area, 2) well 29-4 located upstream from <br />the permit area and 3) [he USGS well, located immediately downstream of the permit <br />area. Also, the Engleville Mine Discharge, called EMD, has also been sampled on an <br />ongoing basis. The initial sampling vas done as part of the small operator's assistance <br />program administered by the Division to help small operators with collecting baseline <br />permit information. Please refer to the groundwater well map in the approved permit for <br />the locations of all wells. <br />Data is available for depth from ground surface, pH, specific conductance, total <br />dissolved solids; total hardness and all ions required by the Division in its groundwater <br />• testing suite. The Colorado Analytical Laboratory in Brighton, Colorado has conducted <br />all testing since baseline data was gathered in the summer of 1988. They have used <br />EPA approved testing methodology in all of the analyses since testing began. All lab <br />analysis used in this report is included in Appendix 1. Data is available from the <br />summer of 1988 to the end of 1994, although it should be noted that there is a gap in <br />testing from 1990 to 1992 when the process of permitting the mine vas taking place. <br />After a short time in operation, the mine was reclaimed in 1993 and final topsoil <br />replacement and revegetation was done in 1994. The mine only disturbed the permit <br />area west of Engleville Gulch; the eastern part of the permit area was never mined. <br />Data Analysis <br />All wells are located in the Vermejo Formation immediately above the Trinidad <br />Sandstone. The Vermejo is composed of thin bedded shales, sands and siltstones <br />interbedded with many split seams of coal. The Formation is approximately 200 to 250 <br />feet thick in the area and dips approximately 1 ° to the west. The Rimrock Mine <br />attempted to mine the same Starkville seam that was extensively mined in the very <br />large underground mine called the Engleville Mine, whose shallow workings were <br />encountered while opening the Rimrock pit. These workings surround the Rimrock pit <br />on all sides except to the north, where the Starkville seams outcrop in the northern half <br />• <br />?.07(1) Page9 1/12/95 <br />`Z <br />