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2012-03-06_REPORT - M1974004
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2012-03-06_REPORT - M1974004
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Last modified
8/24/2016 4:54:46 PM
Creation date
3/6/2012 2:31:01 PM
Metadata
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Template:
DRMS Permit Index
Permit No
M1974004
IBM Index Class Name
REPORT
Doc Date
3/6/2012
Doc Name
ANNUAL FEE/REPORT
From
LAFARGE WEST
To
DRMS
Permit Index Doc Type
Annual Fee/Report
Email Name
TAK
Media Type
D
Archive
No
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Martin Marietta Materials <br />Spec -Agg Project <br />6.0 SUMMARY AND CONCLUSIONS <br />The results of the structural geologic evaluation for the Spec -Agg Quarry, which includes field observations, <br />historic performance, geologic mapping and stereographic analysis of structural geology data; indicate that <br />the current quarry configuration appears to be stable under the existing conditions and current rock mass <br />assumptions. The stability of each of the slopes is enhanced by the absence of significant hydrostatic <br />pressures, by current mining procedures and by the current reclamation process being implemented by <br />Martin Marietta at the site. <br />F -3, the additional foliation set was initially identified in the 2005 study. To date, not enough data have been <br />collected to fully develop a hypothesis regarding the location, extent and properties of the foliation; or to <br />eliminate the possibility that F -3 is basically a signature of the undulating nature of the existing foliation set. <br />The stereographic analysis indicates that the F -3 discontinuity plane may only have minor influence on the <br />south walls and will not influence the north, west or east walls. <br />Evaluations will be conducted during future investigations to assess whether or not any of the foliation sets <br />(F -1 through F -3) are caused due to localized faulting that may have resulted in "structural regions" that have <br />created areas in which the varying orientation of the foliation planes occur. These questions will continue to <br />be addressed as more data are collected. <br />With respect to the quarry walls, the north walls are currently being mined at a slope angle of approximately <br />35° and are currently stable; and as stated in previous reports the slide that occurred on the northeast wall <br />has shown no signs of continued movement since the steepness of the wall slope was modified in 1999. <br />Based on data collected from boreholes in the 2003 geotechnical investigation, a number of relatively <br />shallow foliation surfaces will be encountered below the current main pit elevation of 6,325 feet, starting at an <br />estimated depth of 6,325 feet and the north walls should be monitored closely as the final 20 feet of <br />excavation occurs. <br />The remaining walls are also considered to be currently stable, though the present analysis for the west wall <br />and both the southwest and southeast walls each indicate the possibility for wedge failures, and possibly <br />planar failures, to occur. These two walls of the quarry should continue to be monitored closely as mining <br />continues. As documented in the past, localized raveling, especially along the south walls is likely to <br />continue. Continuation of the safety- minded policies already in place, which limit the height of the exposed <br />highwall, as well as the reclamation of exposed highwalls as soon as possible following blasting and rock <br />haulage, will aid in minimizing the potential for instabilities to occur. <br />February 13, 2012 <br />Project 11361017.00 <br />Page 14 <br />Lachel & Associates, Inc. <br />©2012 All Rights Reserved <br />
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