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February 3, 1993. In March of 1993, the Division verified PCC' s resolution of <br /> many of the adequacy concerns and identified those concerns still requiring <br /> resolution. Powderhorn Coal Company responded with the requested information <br /> received by DMG on March 18, 1993. The Colorado Department of Health (CDOH) <br /> had required PCC to submit a study addressing management of salt loading to <br /> the Colorado River via the Roadside and Cameo operation. Results of the study <br /> were submitted to the DMG on March 1 , 1993, and are entitled "Evaluation of <br /> Alternatives for Management of Salt in Mine Water Discharge. " <br /> The Office of Surface Mining ' s Applicant Violator System (AVS) was queried on <br /> July 18 and 20, 1992 to verify compliance with Rule 2 .03.4 by PCC' s owners and <br /> controllers , and an "issue" recommendation was received. The AVS system was <br /> again checked on May 14, 1993 , and "conditional issue" was recommended. <br /> Additionally, notification was sent to all states in which Powderhorn' s parent <br /> company, Peabody Holding Company, operates coal mines , on February 16, 1993. <br /> One response was received from the State of Kentucky, Department of Surface <br /> Mining Reclamation and Enforcement, verifying that the permittee is not <br /> blocked from receiving a permit in the State of Kentucky. No other responses <br /> were received by DMG. <br /> Description of the Environment <br /> The Roadside/Cameo Mine complex lies in the alluvial valley of the Colorado <br /> River along Interstate 70 just east of the town of Palisade. Located 12 miles <br /> from Grand Junction, the mines are situated in DeBeque Canyon in the <br /> Bookcliffs , a ridge trending Northwest that is comprised of vari-colored <br /> shales and sandstones . The Bookcliffs border the Grand Valley to the east <br /> where the Colorado River exits the highlands of the cliffs and enters the <br /> valley. Mount Garfield, a prominent peak in the Bookcliffs , lies southwest of <br /> the mine site and serves as the southwestern corner of the Piceance basin to <br /> the north . The mines can be located on the USGS 7. 5 quadrangle maps labeled <br /> "Cameo" and "Palisade. " <br /> Structurally, the Bookcliffs coal field is characterized by a monoclinical <br /> structure with the strata dipping gently to the northeast. Exhibits 13 and 14 <br /> of the permit application illustrate the surface geology and structural nature <br /> of the permit area. The mines ' surface facilities are located on and adjacent <br /> to the alluvial valley floor of the Colorado River . The river alluvium ranges <br /> from a clayey to silty sand and contains scattered gravel and cobble-sized <br /> fragments . The depth of the alluvium ranges from nine to sixty feet beneath <br /> the surface disturbed areas . <br /> Historically, the valley has been mined for coal since the late 1800' s , so the <br /> alluvial valley floor has been altered and affected by these operations . The <br /> Cameo power plant, the customer for mined Roadside coal , lies just west of the <br /> mine site along Interstate 70. The valley has been designated as industrial <br /> land use with the alluvial disturbance grandfathered into the permit area . <br /> Nearly the entire surface of the permit area consists of the Mesaverde <br /> Formation, a sequence of interbedded shales , siltstones and sandstones , <br /> indicative of a marine depositional environment. Further to the south, the <br /> Wasatch and Ohio Creek Formations outcrop on the surface . <br /> -5- <br />