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2008-11-24_PERMIT FILE - C1996083 (19)
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2008-11-24_PERMIT FILE - C1996083 (19)
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Last modified
8/24/2016 3:38:13 PM
Creation date
2/24/2009 9:51:39 AM
Metadata
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Template:
DRMS Permit Index
Permit No
C1996083
IBM Index Class Name
Permit File
Doc Date
11/24/2008
Doc Name
Final Geotechnical Invegistation & Evaluation Report, YEH & Assoc, 4/5/06 (Rev. 11/6/2006)
Section_Exhibit Name
Volume IIIA Tab 20 Final Geotechnical Investigation & Evaluation Report
Media Type
D
Archive
No
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Bruce Park Landslide Project No. 25-196 <br />Bowie Mine #2 <br />0 SITE INVESTIGATION <br />Piezometers <br />Four piezometers were installed at the approximate locations presented on Figure 2. <br />Summary logs of the soils encountered are presented in Appendix A. The piezometers were <br />installed to depths of 15 to 22 feet. Groundwater was encountered at a depth of about 17.7 feet <br />in Boring P-2 during drilling. The piezometers were checked on the dates shown in Table 2. <br />The data indicated that spring snow melt may be influencing groundwater levels locally. <br />Groundwater monitoring will continue indefinitely. A summary of the current piezometer data is <br />presented in Table 2. <br />Table 2 - Piezometer Data <br /> Piezometers <br /> P-2 P-4 P-6 P-8 <br />-Approximate Ground <br />Elevation (feet) 8199 8250 8257 <br />I 8221 <br />Date Water Level Below Ground Surface (feet) <br />2-28-06 D D D D <br />3-11-06 D D D D <br />3-17-06 D D D D <br />f <br />1 <br />3-22-06 14.25 D D D <br />3-31-06 10.16 35.93 13.43 _ <br />D <br />4-07-06 4.90 12.67 12.50 D <br />4-14-06 -0.16 12.62 12.28 D <br />4-20-06 -0.22 13.10 12.38 17.71 <br />4-25-06 0.01 13.42 12.61 17.63 <br />5-05-06 2.64 13.83 13.40 20.02 <br />5-31-06 7.85 13.96 14.67 21.14 <br />7-06-06 11.65 13.95 14.67 D <br />Variations in groundwater conditions will likely occur seasonally. The magnitude of the <br />variation will be largely dependent upon the amount of spring snowmelt, duration and intensity <br />of precipitation, and the surface and subsurface drainage characteristics of the surrounding <br />area. Perched water tables will likely develop during spring runoff. <br />Inclinometers <br />Four inclinometers were installed adjacent to the piezometers at the approximate <br />locations presented on Figure 2. The subsoils encountered in the inclinometers were similar to <br />the materials encountered in the piezometers. The inclinometers were installed to depths of 10 <br />to 26 feet below the ground surface into very hard bedrock. The inclinometers indicated <br />4
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