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Similar to other parts of the world, landslides are not a new phenomenon in Africa. They have been reported in Cameroon, Kenya, Uganda, Rwanda, Tanzania, and Ethiopia (Moeyerson 1988; 1989a; 1989b; Davies 1996; Westerberg and Christiansson 1998; Ngecu and Mathu 1999; Ingang’a and Ucakuwun 2001; Muwanga et al. 2001; Knapen et al. 2006). The East African region which includes Malawi, is a heterogeneous in terms of physiography, geomorphology and rainfall, and has a high susceptibility to slope movement. The high annual rainfall, high weathering rates, deforestation and slope material with a low shear resistance or high clay content are often considered the main preconditions for landslides (Knapen et al. 2006).

Landslide Inventory and Susceptibility Assessment for the Ntchenachena Area, Northern Malawi (East Africa)