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The complex nature of creep movements on steeply sloping ground in Southern Rwanda
Authors:Jan Moeyersons
Institution:Royal Museum of Central Africa, B-1980 Tervuren, Belgium
Abstract:Long term soil creep motion is often represented as a type of laminar flow, with velocity vectors parallel to the slope and constant in time. Records on a hillslope in Southern Rwanda reveal that creep movements there compare more with turbulent flow, characterized by a A1 humic horizon superlayer, creeping over a subsoil affected by more irregular creep deformation.
Keywords:Creep  Young-pit  Creep line  Slide plane
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