Skip to main content

Geological Hazards and Anthropogenic Impacts on the Environment in Malawi: Lesson from a Case Study of Debris Flows in Zomba

  • Chapter
The East African Great Lakes: Limnology, Palaeolimnology and Biodiversity

Part of the book series: Advances in Global Change Research ((AGLO,volume 12))

Abstract

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 reconstruct the old events using geological, geomorphological and dating methods and based on these results, 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 metamorphic gneisses and granulites. Weathering erosion and uplift have left the syenite standing at an elevation of 2000 meters while the surrounding area is between 700 and 1000 meters above sea level. Zomba town is located at the foot of the mountain. Steep slopes with up to 50°, the highly jointed syenite, and the thick lateritic soil covers are the main factors likely to influence rock instability. Debris flows triggered by heavy rainfall have affected Zomba since memorial times. People of Zomba and the authorities are well aware of past landslides and the continued risk. As a result from our investigations the detailed risk zoning of Zomba contributes to the disaster preparedness plan of the town.

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 169.00
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book
USD 219.00
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info
Hardcover Book
USD 219.99
Price excludes VAT (USA)
  • Durable hardcover edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

Preview

Unable to display preview. Download preview PDF.

Unable to display preview. Download preview PDF.

References

  • Bloomfield, K. (1965) The Geology of the Zomba area. - Geological Survey Department, Malawi, Bulletin No. 16, Government Printer, Zomba.

    Google Scholar 

  • Carter, G.S. and Bennett, J.D. (1971) The Geology and Mineral Resources of Malawi. - Geological Survey Department, Malawi, Bulletin 6, Government Printer, Zomba.

    Google Scholar 

  • Ingram, J.H. (1946) Procedures of an inquest held before 2nd class magistrate, Zomba.

    Google Scholar 

  • Johnson, T.C., Barry, S.L., Chan, Y. and Wilkinson P. (2001) Decadal record of climate variability spanning the past 700 yr in the southern tropics of East Africa. Geology, 29 (1), 83–86.

    Article  CAS  Google Scholar 

  • Meteorological Department (1973) National Tropical Cyclone Warning Procedures of Malawi, Blantyre.

    Google Scholar 

  • Poschinger, A., Cheyo, D.R.C. and Mwenelupembe, J.J. (1998) Geohazards in Zomba and Michesi Mountain areas. commissioned project report, Hanover.

    Google Scholar 

  • Sitaubi, L.A., Mtambo, P. and Makungwa, S.D. (1996) Forestry development and stream flows on Zomba Plateau. Forestry Research Institute of Malawi Newsletter No. 78, Zomba.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 2002 Kluwer Academic Publishers

About this chapter

Cite this chapter

Mwenelupembe, J., Mylius, HG. (2002). Geological Hazards and Anthropogenic Impacts on the Environment in Malawi: Lesson from a Case Study of Debris Flows in Zomba. In: Odada, E.O., Olago, D.O. (eds) The East African Great Lakes: Limnology, Palaeolimnology and Biodiversity. Advances in Global Change Research, vol 12. Springer, Dordrecht. https://doi.org/10.1007/0-306-48201-0_24

Download citation

  • DOI: https://doi.org/10.1007/0-306-48201-0_24

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-90-481-6083-9

  • Online ISBN: 978-0-306-48201-4

  • eBook Packages: Springer Book Archive

Publish with us

Policies and ethics