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REV13657
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Entry Properties
Last modified
8/25/2016 1:24:46 AM
Creation date
11/21/2007 10:44:27 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981010
IBM Index Class Name
Revision
Doc Date
10/6/1998
Doc Name
TRAPPER MININE INC PN C-81-010 TR 78 1997 ANNUAL REPORT
From
DMG
To
TRAPPER MINING INC
Type & Sequence
TR78
Media Type
D
Archive
No
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Forest Luke <br />Trapper Mining Inc. <br />October 6, 1998 <br />Page 2 <br />Table 1-Hydrologic monitoring data missing from 1997 annual report <br />Sample site Missing <br /> parameter <br />Outfall 013 Metals on list <br /> A-3 in second <br /> half of yeaz <br />Outfalls 015 and Metals on list <br />017 A-3 not <br /> reported for <br /> only discharge <br /> (9/22/97) <br />Wells GB-1, GB2, Fall water level <br />GB-5 <br />Wells GF-4, GF-5, Chromium and <br />and GF-7 radium <br />All GC, GD, GE, PO, and NO, <br />and GF wells <br />Surface water -Compliance with NPDES limits. Trapper's dischazges exceeded the <br />mine's NPDES limitations on six days in 1997. None of the exceedances constituted a <br />violation of an effluent limitation, however, because each exceedance qualified for a storm <br />exemption. Trapper's dischazges were also in compliance with receiving stream standazds <br />set by the Colorado Water Quality Control Commission. <br />Surface water -Impacts from mining <br />4. TDS discussion: Pre-mining vs. post-mining, page 6-6, 2nd paragraph. The third <br />sentence in this pazagraph says: "The TDS of the surface water from the mine azea is <br />similaz to the TDS from the non-mined azea, therefore, an increase has not been defined." <br />Assuming this statement refers to the non-mined S-1 site and the mined NPDES 001 and <br />002 sites, is the conclusion still valid given that flows at S-1 have greatly declined over <br />the yeazs, while flows at NPDES 001 and 002 have shown little change? Could it be that <br />the TDS increase at S-1 was caused simply by diminishing flows, while the TDS increases <br />at 001 and 002 aze caused by a local influx of dissolved solids? <br />5. Long-term TDS trend in No Name Gulch. The attached Figure 1 shows that TDS <br />levels in No Name Gulch have generally increased since the mid-1980s. From late 1984 <br />through 1997, TDS levels above 2000 mg/I have became more prevalent while levels <br />below 1500 mg/l have become less common. At least part of this increase may have been <br />
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