A scree (talus) slope is characterized by an inclined accumulation of rock debris sourced from the upper part of a weathered cliff at the foot of the cliff. Scree slopes are widely encountered in high, frigid mountainous regions and have some interesting geomorphic features (Caine, 1969;Kirkby & Statham, 1975;Sass, 2006). The formation of scree slopes, as shown in Figure 1, is a complex process that involves the detachment, descent, movement, and accumulation of weathered and failed rock. The mechanics of this dynamic process have been of long-standing interest in a number of fields (e.g.,