Uppermost scarps of the slides extend into and beyond areas underlain by Fairview Formation and form a crudely scalloped upper boundary within the colluvium. The upslope ends of the landslides are broad amphitheaters with generally smooth slopes. Over most of the area, the scarps are expressed as a slight but continuous break in slope. The portion of the landslide on the Fairview Formation contains widely scattered benches and ramps that are subparallel to the topographic contours. These benches appear to be remnants of slide blocks that have detached from the scarp and been smoothed over time.