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Abstract
A group of complex landslides in the Razorback area, Australia is described. They are located on hillslopes underlain by Triassic shales and sandstones, on grazing land derived from earlier woodland. The slide types range from debris slides and slumps to earthflows and mudflows. Continued landsliding has been reported since the 1880's until the present. The influence of land use and of annual and daily rainfall on triggering of the landslides is discussed.