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Pennsylvanian-age Belden formation. Outcrops of the Belden appear below the existing quarry <br /> as well, unconformably overlying the Leadville Limestone. <br /> Mid Continent Limestone Quarry Geology <br /> Leadville Limestone in the location of active mine operations is mapped by Kirkham et al. as <br /> dipping between 24 and 38 degrees to the south-southwest, which forms dip slopes and tends <br /> to control hillside slope topography. A series of roughly east-west trending normal faults <br /> crosscut the area but are not mapped as continuous across the proposed expansion area. These <br /> structures are likely a westward extension of the normal-oblique Grizzly Creek Shear Zone, and <br /> the secondary influence on the site's rock mass, outside bedding. <br /> Previous analysis of the Leadville Limestone performed for RMRA indicates the coarse <br /> crystalline rock is composed of 90%to 98% calcium carbonate and low in both magnesium <br /> chloride and silica. Boreholes completed by Colorado Fuel & Iron Corporation (CF&I) in the <br /> 1950's and 1960s were provided by RMRA to WE as scanned hardcopy with approximate <br /> locations. Borehole Lynx 05-001 in the area of the ground event describes the upper 36 feet of <br /> the rock as follows: <br /> Upper Leadville Limestone, med to dark gray, hard, fine grained, some <br /> recrystallized; numerous fractures in all directions re-cemented with w/ <br /> white, yellow, brown, & pink calcite. Some limonite stain, Good acid <br /> reaction. Porous zones at 28-0 to 28-5 and 29-9 to 30-6. <br /> Lower in section, thin mud seams are identified at 51-9 and 58-3, but no description of soft <br /> interbeds are included. <br /> Also of significant note to the modeling of the recent ground event, 1966 borehole Lynx 05-099 <br /> drilled vertically in the area of the event identifies dip in the upper 40 feet of the section as 40 <br /> degrees. <br /> Site Topography <br /> RMR Aggregates, Inc. has developed a very detailed site topographic map, which shows a <br /> moderately-steep, south-facing slope. Slope topography decreases upslope, from south to <br /> north, along the top of the fold. The topography lays back from 1.4:1 at the southern extent at <br /> the existing quarry highwall to roughly 2.5:1 moving uphill 220 yards towards the potential area <br /> of proposed long-term stabilization. <br /> SITE RECONNAISSANCE <br /> January 26, 2023 -Site Reconnaissance <br /> The aforementioned site reconnaissance performed eight days following the ground failure was <br /> primarily an overview of the event, documenting existing conditions and formulating a plan <br /> across represented disciplines to evaluate and stabilize the ground event. Photos with detailed <br /> captions from the reconnaissance are included in Appendix A. Photo 1 shows an overall view of <br /> the ground event on the west face that released along a northeast dipping joint with high to <br /> Page. 2 <br /> 535 161h STREET,SUITE 620 1 DENVER,CO 80202 1 (303)732-3692 1 WWW.KILDUFFUNDERGROUND.COM <br />