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BRIERLEY <br /> ASSOCIATES <br /> Creating Space Underground <br /> August 29, 2019 <br /> File No.: 514104-001 <br /> Asphalt Paving Co. <br /> 14802 W 44th Ave <br /> Golden, CO 80403 <br /> Attention: Stan Opperman <br /> Subject: Geotechnical Stability Report <br /> Ralston Quarry <br /> Golden, Colorado <br /> Brierley Associates (Brierley) has conducted a geotechnical stability evaluation on August 23, <br /> 2019 for the Asphalt Paving Co. (APC's) rock quarry located at 6569 Highway 93, just west of <br /> the intersection with West 64th Parkway, in Golden, Colorado. Brierley has previously produced <br /> a Geotechnical Evaluation and Initial Opinion Report— Phase 1, dated August 2011, a <br /> Geotechnical Evaluation Report- Phase II, dated November 2013, and an Additional Slope <br /> Evaluation letter, dated July 2014 for the same site. <br /> Based on discussions with APC and Greg Lewicki and Associates, PLLC, Brierley understands <br /> that the Division of Reclamation, Mining and Safety(DRMS) has added a geotechnical stability <br /> report as part of the annual reporting. This letter presents the results of this evaluation. The <br /> extent of this evaluation was limited to the basalt quarry and does not include any peripheral <br /> areas. <br /> 1.1 Existing Conditions <br /> 1) Provide an accurate description of the existing high-wall material(s), geotechnical <br /> characteristics, bench, and wall configuration. <br /> According to bedrock geologic maps of the area, the quarry is operating within the western half <br /> of the Ralston Dike, or Ralston Plug. Lava was extruded through the Pierre Shale from the <br /> Ralston Plug during Paleocene time. An altered zone of the Pierre Shale is adjacent to the <br /> Ralston Plug. The contact between that Pierre Shale and the rim-phase of the Ralston Plug is <br /> mapped within the quarry as dipping from 60 to 80 degrees to the east(Drewes, 2006). The <br /> core-phase of basalt is towards the center of the Ralston Plug. <br /> In general, a thin veneer of basalt overlaying the east-dipping shale contact was left in place on <br /> the west side during mine operations. A few"windows" of the altered Pierre shale have been <br /> exposed in the upper high walls and appear to be standing well where exposed. Based on 2010 <br /> mapping, and subsequently reviewed, the rim-phase basalt is very hard, fresh, gray, and very <br /> fine grained, with joint orientation ranging from moderately dipping to vertical. The core-phase <br /> basalt was hard, moderately weathered to fresh at depth, light gray, and very fine grained, with <br /> joint orientation ranging from low angle to high angle. <br /> 990 S. Broadway,Ste.222, Denver,CO 80209 1303.703.1405 1 www.BrierleyAssociates.com <br />