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2014-12-05_HYDROLOGY - M2012032
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2014-12-05_HYDROLOGY - M2012032
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Last modified
8/24/2016 5:55:50 PM
Creation date
12/5/2014 2:50:04 PM
Metadata
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Template:
DRMS Permit Index
Permit No
M2012032
IBM Index Class Name
HYDROLOGY
Doc Date
12/5/2014
Doc Name
Investigation Report of Sediment Laden Water Discharge at Revenue Mine in October, 2014.
From
Greg Lewicki
To
DRMS
Permit Index Doc Type
Hydrology Report
Email Name
RCO
Media Type
D
Archive
No
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The raise bore is drilled through the San Juan Formation of tertiary age and the rock penetrated is <br />primarily andesite, which is a volcanic rock consisting of plagioclase feldspar, quartz and biotite mica. <br />Some limestone is also present in the andesite of this area. The grain sizes are extremely small since <br />the molten rock cooled very rapidly. Normally, the rock has a subdued greenish color, but occasionally, <br />a slight iron impurity will color the rock with a reddish color. <br />4. Reasons for Sediment Laden Discharge <br />During the drilling of the pilot hole from the surface, no appreciable water was observed in the hole, so <br />no extra precautions were taken to address water at the bottom of the raise bore. After the 8 feet bit <br />was attached and the raise bore progressed upwards, a zone of rock was encountered that did have <br />more water than anticipated from the pilot hole. By coincidence, this area also had a zone of andesite <br />that had reddish color and some of the plagioclase feldspar had converted to minor amounts of clay <br />over thousands of years. <br />Any water produced from the raise bore would enter the Virginius workings and then the ditch along the <br />main Revenue Tunnel and flow by gravity an additional 7900 feet to the mine portal. At that point, the <br />water entered two 8" diameter HDPE pipes which discharge into Sneffels Creek. Once the mine is in <br />full operation, these discharge pipes will enter the Mine Water Pond and this water will discharge into <br />Sneffels Creek. This is expected to occur in December of 2014. <br />During the early morning hours of October 24, the raise bore encountered this zone of higher water flow <br />and reddish color andesite. This water was later estimated to be approximately 20 -25 gallons per <br />minute. As the water trickled down the raise bore and passed through the finer material from the drilling <br />of the raise bore, sediment laden water was produced. This water combined with the normal clear water <br />flow from the mine of approximately 250 -300 gallons per minute and this water was discharged to <br />Sneffels Creek. <br />Page 6 of 17 <br />
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