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^III IIIIIIIIIIIII III <br />999 <br />Harding lawaon llsaoelatsa <br />November 30, 1995 <br />HLA #32640.14 <br />Mrs. Kathy G. Welt, Environmental Supervisor <br />Mountain Coal Company <br />West Elk Mine <br />P.O. Box 59l <br />Somerset, Colorado 81434 <br />RE: FACTOR OF SAFETY SCTMMATION FOR THE PARKING LOT EXTENSION AT THE <br />WEST ELK MINE <br />Dear ~~Y <br />The following letter summarizes the factors of safety for the parking lot extension located to the <br />south of the present parking tot at a general elevation of 6320 feet above mean sea level. The parking lot <br />extension and adjacent cut slope is 50 feet wide by 360 feet long, and extwds to the south of the present <br />parking lot. The total surface area of the parking lot ext®sion including the cut slope area is <br />approximately 17,500 square feet. The following pazagraphs describe the slope stability analysis required <br />for permit submittal. <br />A slope stability analysis was performed on two profiles extending up the slope on either end of <br />the proposed parking lot extension. The first set of calculations determine the fattors of safety prior to <br />exravation of the parking lot extension. The second set of calculations determine the factors of safety <br />after the parking lot has been completed. The slope stability analysis utilized the PCSTABLS program to <br />determine the factors of safety against failure. The factor of safety is the ratio of the forces resisting the <br />slope movement to the forces which cause the slope to fail. The resisting forces are determined by the <br />shear strrngth of the native soils to resist failure along a specific surface. The forces which tend to cause <br />failure include; but aze not limited to: (a) the angle of the slope; (b) the location of existing access roads <br />and drainage ditches in relation to the slope; (c) pore pressure or water table atting on the failure plane; <br />and (d) the charatteristics of the native soil and bedrock found is the slope. A factor of safety of l.0 <br />implies that the slope is mazginally stable for the cross-section profiles, native clay/topsoil material <br />strengths, groundwater, and the slope conditions. As required by the State of Colorado Mined Land <br />Reclamation Board, 1991, a minimum factor safety of l.3 will be requved for the cuVfill slopes of the <br />parking lot extension. <br />It was concluded that two unrelated slope failures could occur at this site based on observations in <br />the field, borehole information, and previous experience in this area. Looking to the south, or uphill from <br />the present parking lot, the first failure would occur in the east half of the slope in the area designated as <br />Qlsl (refs to figure 1). The second soil failure would ocnrr in the western half of the slope in a second <br />area designated as Qlsl. Qlsl is defined as a surficial slump or weep involving the over burden soils and <br />thin seams of bedrock. It is characterized by hummocky or boulder strewn topography. Qlsl soil <br />compositions ranges from clays to gavel derived as slope wash and residual soils. <br />A description of the criteria uses in the P~~" 'BLS prnera~ *o evaluate the facors of safety for <br />the proposed mar .! storage •a ~s as follows: <br />O' . hoot ~eometrv: The resent slope profiles w Ke ~veloped rsom a 1992 aerial -opogaphy <br />map supplied by Mountain Coal Company. <br />Groundwater: Groundwa .- was assumed at approximately IS feet below surface, and has been <br />previoLLSly identified as two springs in the slope above the parking lot extension at the general <br />Engmeenng ana t76 East $mih Temple. $wca 1570. Salt take Clry. Utan Ban! Te~eonone: 18011 36&~55 ieleccoy: X90:. 753s.:;5 <br />EnvllOrlTenid $erviCeS Ib,nva nn .q H.mn•~c.r~...uun,.•v •,~~..,,,,,,,~i~ <br />