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REP33262
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REP33262
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Entry Properties
Last modified
8/25/2016 12:09:33 AM
Creation date
11/27/2007 6:27:43 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981010
IBM Index Class Name
Report
Doc Date
3/18/2005
Doc Name
2004 AHR Section 2.5 Parts 1.0 to 7.0 Appendix A
From
Trapper Mining Inc
To
DMG
Annual Report Year
2004
Permit Index Doc Type
Hydrology Report
Media Type
D
Archive
No
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• <br />Steady water levels were observed in the last four years in well GMP-1 with the previous <br />ten years showing a water level rise due to the movement of Pit A to the east of this azea No <br />dewatering was produced from the Z pit in 2004 while some dewatering occurred from the F pit. The <br />fairly steady water levels in well GD-3 in 2004 indicate that rechazge was large enough to maintain this <br />level. The water levels in KLM well GP-2 overall gradually declined in 2004 after a previous water <br />level rise that followed a larger decline. The previous decline could have been caused by the decrease <br />in rechazge and mining in this area <br />Water-level changes aze discussed in more detail in the following section. <br />2.1.2 WATER-LEVEL CHANGES <br />Water-level changes for 2004 are presented in Figures A-1 through A-14 in Appendix A. <br /> <br />The table in Appendix A list all historical data for the Trapper Mine. The wells are grouped on the <br />water-level plots according to aquifer where possible but, in most cases, aze grouped by similar water- <br />level elevations. Table A-1 in Appendix A presents a tabulation of the water-level elevations for each <br />of the monitoring wells. Figure 2-1 presents the total annual precipitation at the Trapper Mine from <br />1978 through 2004. Precipitation declined from a high in 1983 to a low in 1988 and had increased <br />agaui to a peak in 1993 with a below average vah>e in 1994. The yeazs 1995 through 1997 had above <br />average precipitation relative to the Trapper Mine record, while 1998 through 2004 were below. The <br />precipitation in 2004 was 2.7 inches below normal. Water levels in rriarry of the wells reflect the natural <br />variations in rechazge. These changes may lag the actual precipitation events due to the time it takes <br />the head change to move through the aquifer to the monitoring we1L <br />Wells GP-5 and GP-6 aze useful in defining natural variations in the QR aquifer for 2004. <br />Water levels in wells GP-5 and GP-6 show a rising trend from 1995 through 1998 with an overall <br />gradual rise from 1998 to 2002. Water levels in these two wells have been fairly steady the last three <br />Trapper Mining Company <br />2004 Mnual Report <br />
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