Hydroclimatic trends, sediment sources and geomorphic response in the Bell River catchment, eastern Cape Drakensberg, South Africa
The Bell River in the Eastern Cape Drakensberg of South Africa has shown recent signs of channel instability as evidenced by avulsion, sinuosity reductions, gradient steepening and general channel instability. Analysis of rainfall data did not provide evidence for progressive long term change in rai...
| Main Authors: | , |
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| Format: | Others |
| Language: | English |
| Published: |
1995
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| Online Access: | http://hdl.handle.net/10962/d1006655 |