Gravitational slope processes on the southern coast of the Crimea

Abstract

A paragenetic assemblage of gravitational processes takes part in slope modelling at the Southern coast of the Crimea, including rock falls, scree sliding, landslides and creep. The processes are elements of the complete cycle of slope formation, the rock and soil being involved into movement gradually, starting from the sea coast and proceeding to the Crimean Plateau (Yayla). Individual landforms evolution may be controlled by technogenous factors as well as by natural ones. Slopes morphoelements are discussed, which are characterized by 'certain gravitational processes and resulting landforms.