Analyses of Valley Fill Slope Stability - Three Case Studies

Surface mining of multiple scams by mountaintop mining methodology is complex in the Appalachian region of West Virginia. Excess spoil from the removal of overburden and interburden is disposed in the adjacent valleys. The valley fills so formed are some of the largest earth constructions, with a relief of 450 ft (137 m) to 650 ft (198 m) and a stretch of 500 ft (152 m) to 2000 ft (610 m). The stability of the valley fills has become an issue of public concern. This paper describes three cases of valley fill slopes. The analysis of each case involved the description of the geo-mechanical properties of different surface and sub-surface layers, and the surface configuration of the slope. Slope stability was carried out using deterministic as well as probabilistic approaches. Based on the analysis, it was found that valley till slopes were stable due to configuration, and the premise that valley fills with great stretch and high volume of spoil tend to be unstable does not hold.