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Geotechnical Stability Exhibit ��� <br /> Engineering Evaluation of Highwall Design for the South Quarry of the Morrison Quarry <br /> 5 Design Methodology <br /> 3-D Geologic Model <br /> A three-dimensional (3-D) geologic model was prepared and submitted to Aggregate Industries <br /> by GEI in 2018, as an update to the 2017 version, and was included in the Permit M-1973-021 <br /> AM-07 Geotechnical Stability Exhibit. As part of this task order, HDR prepared a separate <br /> model incorporating historic data, as well as the recent drilling effort, to better define the <br /> geologic structural conditions of the site. Reserve calculations were not part of this effort. The <br /> HDR geologic model was prepared to visualize the areas of competent bedrock in relation to <br /> areas in which the bedrock was considered lesser strength, and thusly modeled in the stability <br /> calculations as weaker material. In general, based on the results of the petrographic analyses, <br /> the weaker rock is described as Talc-Gneiss; however, the exact mineralogic composition of the <br /> rock in this area is variable and may consist of a percentage of clay mineral assemblages. <br /> Development of the geologic model was performed using LeapFrog Works, version 2022.1.1, <br /> and includes boring data from the previous drilling efforts as well as the recent 2022 HDR field <br /> event. The proposed geometry Iinework was downloaded from the Propellor site, maintained by <br /> Holcim, and includes mapping of 40/40 benches below El. 6600. File was dated December 21st <br /> 2022. <br /> Lithologic mapping included simplifying the boring data by competent material, including biotite <br /> gneiss, granitic gneiss, quartz, etc., as compared to less competent including the previously <br /> described sillimanitic gneiss, talc-gneiss, or gneiss with a combination of intermixed <br /> sedimentary material. Upon simplifying the Iithologies, HDR correlated the materials to estimate <br /> the Iithologic bounds, and included existing mapped exposures to better refine the model. The <br /> resulting model is included in Appendix B, Geologic Model, along with cross sections cut to <br /> show the subsurface conditions at pre-determined station intervals. The model is estimated <br /> based on currently available information and could be refined with additional drilling information. <br /> 5.2 Bench Stability <br /> The simplified geologic model with anticipated 60/40 bench configurations above El. 6,600 and <br /> 40/40 bench configurations from El. 6,600 to current permitted El 6,500, was utilized to evaluate <br /> the current and future stability of the Morrison Quarry as mining proceeds in the South Quarry <br /> below El. 6600'. Evaluations of stability include global and local factors of safety with <br /> RocScience SLIDE2 and FLAC/Slope, as well as kinematic analysis using RocScience DIPS of <br /> planar, toppling and wedge failures based on discontinuity data collected via field visits, high- <br /> density orthoimagery, and downhole geophysics. <br /> 5.2.1 Hoek-Brown Parameters <br /> The 3-D geologic model provides a spatial representation of competent biotite/granitic gneiss <br /> and less competent talc-gneiss. In order to evaluate the stability of the proposed bench <br /> configurations, generalized Hoek-Brown strength parameters were defined based on recent field <br /> May 2023 1 18 <br />