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Reclamation Feasibility Report - Virginia Canyon <br />IL._J <br />INTRODUCTION <br />This report is intended to be a guidance document for use in reclaiming mining sites in Virginia <br />Canyon. The Colorado Division of Minerals and Geology (DMG) inspected approximately 200 <br />mine waste piles in this study. DMG also sampled water quality in 2000 during spring snowmelt <br />and during a summer thunderstorm. In 1999, the Colorado School of Mines (CSM) sampled stream <br />sediments and collected water quality samples during spring snowmelt, low-flow, and following a <br />summer thunderstorm. The water quality, mine waste and sediment data were used in conjunction <br />with site observations to prioritize mining sites for reclamation. The ultimate goal of this work is to <br />reduce metals loading to Clear Creek from Virginia Canyon by reclaiming the mining sites <br />contributing the largest metal load. <br />GENERAL SITE DESCRIPTION <br />LOCATION <br />Virginia Canyon is located in Clear Creek County immediately north of the town of Idaho Springs. <br />Virginia Canyon begins approximately 2 miles north of Idaho Springs. Figure 1 is a general <br />location map of the area. <br />Mining began in Virginia Canyon in 1860 following the discovery of Placer Gold by George Jackson <br />near present day Idaho Springs and the discovery of lode gold by John Gregory near present day <br />• Central City. Gold was the principal product mined in Virginia Canyon; although the mines in the <br />Seaton Mountain area were principally silver. Most of the ores were hauled by wagon to the Idaho <br />Springs area for milling. Most of the larger mines operated until World War II, when a presidential <br />order required cessation of all mines not mining "strategic metals". <br />Investigation of the water quality of Virginia Canyon was initiated as part of an effort to improve the <br />water quality of Clear Creek. Virginia Canyon is one of the largest sources of heavy metals to <br />Clear Creek. The lower portion of Virginia Canyon has perennial flow most years, while the mid- <br />elevations are intermittent, and the upper reaches are ephemeral. Most of the flow from Virginia <br />Canyon enters Clear Creek as ground water. Heavy metals in the flow from Virginia Canyon <br />originate from leaching of eroded mine waste in the stream channel, direct leaching of mine waste <br />piles, and leaching of un-mined sources. <br />BASELINE DATA COLLECTION <br />WATER QUALITY SAMPLING <br />The DMG sampled along Virginia Canyon during a snowmelt event and a thunderstorm event. <br />Twenty-four stream sites and 4 draining mine adits were planned to be sampled (Figure 2). <br />Snowmelt was sampled on May 9, 2000. Because the snow pack was lower than normal, there <br />was very little runoff during May of 2000. A total of 14 stream sites and 3 draining mine adits were <br />sampled. Stream flow was measured using one-inch and four-inch Baski cutthroat flumes. Field <br />measurements included pH and electrical conductivity. Water samples were collected at each site <br />• in 250 ml pre-acidified HDPE bottles. Total recoverable metals and dissolved metals samples <br />were collected. The dissolved metals samples were filtered through 0.45 micron filters in the field.