Solifluction lobes and sheets are types of slope failure and landforms. In solifluction lobes sediments form a tongue-shaped feature due to differential downhill flow rates. In contrasts solifluction sheets sediment moves more-less uniformily downslope, being thus a less selective form of erosion than solifluction lobes.
Solifluction lobes in Wyoming.
Solifluction lobes on a slope devoid of vegetation. Nunavut, Canada.