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2006-12-12_REPORT - M1974004
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2006-12-12_REPORT - M1974004
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Last modified
8/24/2016 3:16:32 PM
Creation date
12/29/2010 7:13:41 AM
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Template:
DRMS Permit Index
Permit No
M1974004
IBM Index Class Name
REPORT
Doc Date
12/12/2006
Doc Name
2006 Geotechnical Report
From
Lafarge North America
To
DRMS
Email Name
ACS
Media Type
D
Archive
No
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<br /> <br /> <br /> <br /> <br />for use in this year's analysis. These poles are summarized in Figure 8 and are <br />presented in further detail in Table 2 below. <br />Table 2: Representative Discontinuitv Orientations <br /> Dip Direction/Dip <br /> 1997- <br />Concen- 2002 & 2003 2003 2005 2006 Entire <br />tration 2004 Main Pit Southern Surface Surface Dataset <br />Center Surface Borehole Expansion Mapping Mapping (2,960 <br /> Mapping Data Data Data Data points) <br /> Data <br />F-1 (Fol) 176°/36° 168°/38° 177°/35° - 157°/39° 159°/35° <br />F-2 (Fol) - - 258°/17° (1) 209°/160 198°/24° - <br />F-3 (Fol) - - - 336°/44° 2940/36° - <br />P-1 (Joint) 174°/81 ° 178°/74° 171 °/75° 172°/76° 165°/72° 171 °/76° <br />P-2 (Joint) 089°/72° 082°/63° 095°/55° 104°/61 ° 102°/47° 0870/63° <br />P-3 (Joint) 257°/73° 256°/66° 248°/53° 255°/61° 257°/79° 2510/68° <br />P-4 (Joint) 293°/72° 294°/70° 316°/41 ° 308°/76° - 2870/70° <br />P-5 (Joint) 334°/86° 349°/62° 343°/73° - 336°/76° 3450/62° <br />P-6 (Joint) 028°/68° 037°/57° 031 °/55° 039°/58° 029°/49° 0280/53° <br />(1) Orientati on of foliation found in the upper 300 feet of boring DH-03-03 <br />2 The orientations in bold were used as representative for this stud <br />Note the overall adjustments shown in Table 2 that have been made to the <br />general orientations for each of the discontinuity (foliation and joint) sets based <br />on the combined discontinuity data obtained over multiple years' analyses. <br />' Overall, the discontinuity sets obtained by analysis of the entire dataset (i.e., <br />2,960 points) are consistent with the cluster analysis from previous years' <br />' individual analyses, with the exception of foliation orientations, F-2 and F-3 <br />(Figure 9). Both of these two discontinuity orientations are identifiable within the <br />quarry, but have not been recorded in large enough quantities to create a strong <br />signature in the analysis of the entire dataset. However, based on the <br />prevalence of these discontinuities in the southern expansion area, both of these <br />orientations have also been used in this analysis. <br />A further analysis of the available cluster data was used to assess the <br />' hypothesis that distinct "structural blocks" exist within the quarry, a cluster <br />analysis showing the poles based on collection areas has been developed <br />-16-
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