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Hudson, C.A. A regional application of SLEMSA in the Cathedral Peak area of the Drakensberg. Unpublished MSc. Thesis, University of Cape Town, South Africa. 1987.

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Article

Erosion Hazard Mapping in the Runde Catchment: Implications for Water Resources Management

1Department of Physics, Geography and Environmental Science, Great Zimbabwe University, Masvingo


Journal of Geosciences and Geomatics. 2013, Vol. 1 No. 1, 22-28
DOI: 10.12691/jgg-1-1-4
Copyright © 2013 Science and Education Publishing

Cite this paper:
Godfrey MUTOWO, David CHIKODZI. Erosion Hazard Mapping in the Runde Catchment: Implications for Water Resources Management. Journal of Geosciences and Geomatics. 2013; 1(1):22-28. doi: 10.12691/jgg-1-1-4.

Correspondence to: David  CHIKODZI, Department of Physics, Geography and Environmental Science, Great Zimbabwe University, Masvingo. Email: dchikodzi@hotmail.com

Abstract

Soil erosion not only makes agricultural lands unproductive, it also contributes to sedimentation of water bodies leading to the eventual filling up of these water bodies. The control of sedimentation in reservoirs requires that the potentially significant sources of sediments be known and characterised. Knowledge of the spatial variations in the erosion hazard of a catchment is a good starting point. Using the Soil Loss Estimation Model for Southern Africa (SLEMSA) within a Geographic Information System (GIS), we characterized the spatial variations in erosion hazard in the Runde catchment in Zimbabwe. Results from this study show that the greater part of the catchment (around 64%) is in the moderate to negligible erosion hazard classes. Around 17% of the total catchment is in the moderately high to extremely high categories. We concluded that under the current land cover and land use regimes, water bodies in the Runde catchment are not at risk from abnormal rates of sedimentation.

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