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~~.., Illllllllllllllllll ~. <br />.~- <br />STATE OF COLORADO <br />DIVISION OF MINERALS AND GEOLOGY <br />Department of Natural Resources <br />131 J Sherman 51 . Room :1 S <br />Denver, Colorado 80?03 <br />Phnne~ (3031 866-3567 <br />FA%: (3031 83?-8106 <br />DATE: March 28, 2001 <br />TO: Tom Schreiner <br />FROM: Allen Sorenson <br />DIVISION OF <br />MINERALS <br />GEOLOGY <br />RECLAMATION <br />MINING~SA FE TY <br />Bill Owens <br />Governor <br />GregE Watcher <br />Eaecunve D~reaor <br />RE: Protection of Nearb Structures A r ate Industries West Central Re on Inc. M'cnael B Long <br />y + gg ~ + ~ + +Dwlvon Director <br />Fredstrom Resources Pit, File No. M-2001-016 <br />I have reviewed Exhibit S to the above referenced permit application, including the slope stability analysis <br />prepared to demonstrate that nearby structures will not be damaged by mining. The Application states in Exhibit <br />S that agreements will be forged with ditch owners to allow mining in close proximity or directly through existing <br />irrigation laterals and ditches. As such, the permit should stipulate that no mining will occur within 200 feet of <br />ditches and laterals until the agreements have been provided to the Division of Minerals and Geology (DMG) and <br />accepted as part of the reclamation permit. <br />As for the structures other than irrigation ditches, the critical area for analysis of slope stability is at the northwest <br />comer of the proposed gravel mining operation. In the northwest comer, the excavation will be at its deepest, 23 <br />feet according to the drilling logs, and mining will occur at the closest point (50 ft.) to any of the structures in the <br />mine vicinity. The analysis provided in the application models the shale bedrock underlying the gravel layer using <br />relatively high shear strength. This analysis yields a safety factor of 2.1 for the northwest comer of the operation. <br />Typically, the shale bedrock in the azea of the proposed operation will be weathered at the graveUshale contact, <br />and the weathering will extend to a depth of several feet. The residual shear strength of the weathered shale may <br />be much lower than the sheaz strength input to the Applicant's analysis. <br />The DMG has completed an independent analysis of the critical cross section for stability at the Fredstrom Pit. <br />DMG's analysis differs from the Applicant's in that a three foot thick layer of residual strength weathered shale is <br />modeled at the graveUshale contact. The shear strength parameters input for the weathered shale layer are zero <br />cohesion and an internal friction angle of 14 degrees. Also, the DMG's model assumes a near vertical highwall as <br />opposed to the Applicant's modeled O.SH:I V slope. The results of the DMG analysis are attached to this memo. <br />A safety factor of 1.34 is output. Although this safety factor is much less than the 2.1 estimated by the Applicant, <br />it is still sufficient to assure the protection of structures. Particulazly since the 1.34 safety factor results from <br />analysis of the worst reasonable case scenario for both shear strength and highwall angle. <br />Based on the DMG's analysis, the mining limits depicted on the Exhibit C, mining plan map, may be approved. <br />However, since the mining limits do not coincide with the proposed permit boundary, it is important to emphasize <br />that the mining limits depicted on the map are not considered by DMG to be generalized or flexible. Rather, these <br />mining limits and the setbacks from structures stated in the application will be enforceable components of the <br />reclamation permit. As such, the mining limits should be marked in the field prior to commencement of <br />excavation. <br />attachment(s) <br />cc: Carl Mount, w/attachments <br />c:windaws~personalVredavomdoc <br />