| BLYDE RIVER: Hydrology and geohydrology |
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eWISA Home | BLYDE: MAIN INDEX | ALPHABETICAL LIST OF RIVERS | ||||||||||||||||||||||
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Map of the BLYDE River |
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| HYDROLOGY | |||||||||||||||||||||||
| The Blyde River catchment has a high rainfall and the water emanating from the Blyde River makes an important contribution to the base flows in the lower reaches of the Olifants River passing through the Kruger National Park. (Ref 1) | |||||||||||||||||||||||
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"This
sub-catchment consists of the area drained by the |
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"The Blydepoort
Dam is the largest impoundment on the |
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"Flow patterns in
the upper reaches of the Blyde and Ohrigstad rivers are relatively
stable as these rivers drain an area that receives some of the highest
rainfalls recorded in South Africa (average rainfalls in the headwater
regions of these two rivers exceeds 1,500 mm per year).
Both rivers are therefore perennial, though flows increase during
the summer months when rain is received.
Smaller tributary streams in the upper reaches are also
perennial, though their flows are more variable.
In its lower reaches, the |
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| GEOHYDROLOGY | |||||||||||||||||||||||
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| References | |||||||||||||||||||||||
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Ref 1: Department of Water Affairs and Forestry, South Africa. 2004. Olifants Water Management Area: Internal Strategic Perspective. Prepared by GMKS, Tlou and Matji and WMB on behalf of the Directorate: National Water Resource Planning. DWAF Report No P WMA 04/000/00/0304 . "Ref 2" (www.mining.wits.ac.za/FinalReport-Section5.doc) |
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