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2015-03-11_REPORT - M1974004
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2015-03-11_REPORT - M1974004
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Last modified
8/24/2016 5:58:12 PM
Creation date
3/18/2015 9:48:30 AM
Metadata
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Template:
DRMS Permit Index
Permit No
M1974004
IBM Index Class Name
REPORT
Doc Date
3/11/2015
Doc Name
Annual Report Fee Map
From
Martin Marietta Materials, Inc.
To
DRMS
Email Name
MAC
Media Type
D
Archive
No
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Martin Marietta Materials <br />Spec -Agg 2015 Annual Report <br />7.0 CONCLUSIONS AND RECOMMENDATIONS <br />The results of the structural geologic evaluations and kinematic structural discontinuity analyses for the <br />Spec -Agg Quarry do not indicate any immediate concerns with respect to large -scale instabilities in the <br />current final quarry wall faces based on our field observations and current rock mass assumptions. The <br />stability of the slopes is enhanced by the absence of significant hydrostatic pressure, by current mining <br />procedures, and by the current reclamation process being implemented by Martin Marietta at the site. <br />While large -scale failures are not anticipated, the slope will continue to shed rocks (minor raveling) over <br />time as a result of small -scale failures (planar or wedge failure), particularly in near - vertical temporary <br />bench faces. <br />For the 2015 annual report, kinematic analyses are based on discontinuity measurements derived <br />principally from data collected from the existing growing dataset supplemented with data collected during <br />the June and December 2014 site visits. The results of these analyses are not intended to supersede <br />results of analyses performed for prior years that were based on representative discontinuity orientations <br />generated from the entire set of measurements. Rather the analyses presented herein are meant to <br />compliment previous years' analyses and enable monitoring of possible new trends in the data that could <br />result in previously unconsidered failure modes. <br />The collected data for this evaluation was complimentary to and were consistent with past analyses. It is <br />noted that the results for the current analysis did not change the pole or the resultant concentration center <br />for any of the delineated joint sets significantly from any of the recent years' results. In general, the data <br />collected during the June and December 2014 site visits correspond reasonably well with representative <br />discontinuity orientations used in previous reports; however, we noted some minor differences which we <br />applied to our kinematic analyses for the 2015 annual report. <br />The kinematic analysis for East Wall 1, Northeast Walls 2 and 3, Northwest Wall, West Walls 1, 2 and 3, <br />and Southeast Wall each indicate the possibility for wedge failures to occur. Additionally, the analysis for <br />Northeast Walls 1 and 3 shows the potential for planar failure. The walls of the quarry in these areas <br />should continue to be monitored closely as mining continues to assess the potential for the indicated <br />failure modes to contribute to large -scale slope instability of a final mine highwall based on the continuity, <br />regularity and variation in orientations of the discontinuities involved. <br />We also recommend that known faults are tracked and observed in new exposures to confirm orientation <br />and character for supplemental stability analysis, as needed. We expect the southern fault identified by <br />Gable (1968) and in previous years site visits (Figure 3) may be exposed in other locations as <br />excavations continue in the Southern Expansion Area. Additionally, the unmapped fault generally located <br />in the central portion of the quarry may be exposed for mapping in the future. In addition, as <br />recommended in the previous reports, evaluations will be conducted during future investigations to <br />assess whether or not any of the foliation sets (F -1 through F -3) are caused due to localized faulting that <br />may have resulted in "structural regions" that have created areas in which the varying orientation of the <br />foliation planes occur. These questions will continue to be addressed as more data are collected. <br />As documented in the past, localized raveling, especially along the south walls is likely to continue. <br />Continuation of the safety- minded policies already in place, which limit the height of the exposed highwall <br />as well as the reclamation of exposed highwalls as soon as possible following blasting and rock haulage, <br />will aid in minimizing the potential for instabilities to occur. The quarry walls appears to be relatively dry <br />February 25, 2015 Page 16 Lachel & Associates, Inc. <br />Project 14364006 00 02015 All Rights Reserved <br />
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