Abstract
Many South Australian landslides are due to mass movement of hillslope debris and have occurred during periods of intense rainfall. Earth flows, incorporating rotational movement, occur in Permian Sediments on the Fleurieu Peninsula and are due to the effects of land clearing. Massive rotational slumping, occurring in bedded rocks, has been recorded at several localities as have numerous rockslides in quarries, open cut mines, and road cuts.
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