Natural geological hazards such as flash floods, landslides, debris flows and mudflows have caused, and will continue to cause, many problems in Malawi. Landslide risks are primarily a geological problem and it is Quaternary geology that concerns our environment most. It is a typical geological task to rec('ostruct the old events using geological, geomorphological and dating methods and based on these res~lts, predict possible future disasters. Our studies of old and recent debris flow events in Southern Malawi have found out that these phenomena are mainly triggered by tropical cyclones that bring heavy rainfalls. They occur in mountain slopes with certain slope instability, soil cover and discontinuity patterns of the underlying rocks. Human impacts on the environment such as large scale earthworks projects and replacement of natural forests by non endemic tree species have also played an important role in a rising risk of flash floods and debris flows. It is recommended that the most sustainable method of mitigation against these hazards is to incorporate the geological hazard zoning maps into town and regional planning schemes. Where this may not be possible, measures that can reduce or minimise the hazard impact should be adopted. Zomba Mountain is made of a Mesozoic syenite pluton that intruded Precambrian high-grade
CITATION STYLE
Mwenelupembe, J., & Mylius, H.-G. (2002). Geological Hazards and Anthropogenic Impacts on the Environment in Malawi: Lesson from a Case Study of Debris Flows in Zomba (pp. 557–573). https://doi.org/10.1007/0-306-48201-0_24
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