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r ' • <br />• <br />Balaz & Associates <br />New Coal Waste Pile and Haul Road Project, Sanborn Creek Mine, Somerset, CO <br />June 18, 1997 Page 3 <br />Il is possible that the quality of borrow materials may be such that a Geogrid material will have to be either <br />partially or completeh~ substituted for the geotextile fabric. To make this determination, either a lazge number <br />of exploration pits and additional laboratory testing will be required or changes will possibly be made during <br />actual conswction. <br />The fill section at station 27+00 will probably require mechanically reinforced earth in the entire fill. Even <br />though this slope is somewhat flatter than the section at station 8+00, it is anticipated the materials used for <br />construction in this area may contain a significantly higher amount of silt and clay fines and the anticipated <br />colluvial soils at the base and tce area will convol the design. The use of mechanically stabilized soils `forces <br />the projected failure surfaces back toward or into the more competent Bowie Member. It is anticipated the more <br />clayey collucial soil will be used to conswct this fill. The `external wck loading' creates potential failtre near <br />the upper fill face, which can be resisted by the mechanically stabilized earth. <br />The surface exposures oCsandstone and siltstone are expressed on the topography map as relatively steep slopes, <br />which were initialh• avoided for the road alignment. ARer consideration of the increased amounts oC sandstone <br />and siltstone beds in these areas, it is believed the majority of the cut slopes can be steepened to between 1:2 <br />(H: V) to 1:4 (H:V) without sacrificing the integrity oCthese cut slopes. These cut slopes will have to be carefully <br />obsen•cd during the conswction process to determine if any additional stabilization techniques, such as <br />benching, (latter slopes, rock butvess/MSE walls or tie-backs in the worse case aro required. <br />Item 18. Location and T}pe of Fill Slopes LincolnDeVon;andBalaz&Associateshavc <br />jointly developed sheet OXWVF- I G to indicate typical cut and fill sections, slope stabilization and anticipated <br />stationing along the proposed roads for review, bidding and construction purposes. Actual field conditions may <br />require modifications oC this plan. <br />Item 24. Scdimcnt Pond Edward M. Moms. PE, of Lincoln DcVorc was prescnt, during the <br />excavation of an exploration vcnch within the proposed Scdimcnt pond on 9-1 G-9G. Il was our understanding <br />that as this exploration vrnch was being logged by personnel of WESTEC, and that a log of the soil profile and <br />recommendations for the construction of the sediment pond would be forthcoming from WESTEC. Following <br />is our description of this exploration pit. Personnel of Lincoln DeVorc did not obtain any samples for testing <br />and the following descriptions will be based on visual logging only. <br />The exploration pit was situated near the in-flow point of the sediment pons, as indicated on the attached <br />drawing. This drawing is based upon the Plan of the Scdimcnt Pond as depicted on the Plan OXWVF-03. <br />prepared by Balaz & Associates. The total trench was approximately 50 feet long, including minor probing at <br />the upsucam side. near the visible outcrop of the Rollins Sandstone. At the lovvcr, southern end of the vcnch. <br />the naticc debris fan/colluvial material was encountered at a total depth of I S fcet and the Rollins Sandstone <br />surface had fallen below the maximum reach of the backhce bucket. At approximatcl}' 10 feet below the ground <br />surface. some iron/steel debris ryas encountered, indicating the original ground surface ma} have been <br />approximately 10 feel bclo~v the prescnt ground surface. It is bclicccd that some oCthc `recent' fill in this gully <br />is related to construction of the Railroad embankment. At a depth of 6 to 7 feet below the prescnt ground <br />surface, a vrn rocki zone vvas encountered, which does not appear to be man-made fill but appeared [o be part <br />of natural deposits of alluvium and colluvium. The type of svatification, the orientation of the rock and boulder <br />