BREEDE RIVER: Topography, geology and soils

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Map of the BREEDE River

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TOPOGRAPHY
The topography of the Breede Water Management Area is characterised by mountain ranges in the north and west, the wide Breede River valley, and the rolling hills of the Overberg. The Breede valley is flanked by the Franschhoek and Du Toit's Mountains in the west, the Hex River Mountains to the north and the Langeberg Mountains in the east. The higher peaks reach an altitude of 1500m-2000m. (Ref.1)
The topography of the Breede-Overberg area is characterised by the Franschoek and Du Toit's Mountains in the west, the Hex River Mountains to the north and the Langeberg Mountains in the east, with a wide Breede River valley and the rolling hills of the Overberg in the south. (Ref 2)
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The profile of the Breede River (from the origin near Ceres to the mouth at Witsand)  is illustrated below:
    GEOLOGY                                    
Upper Breede:  Quartzitic Table Mountain sandstone, Bokkeveld and Malmesbury shales, Enon conglomerate
Central Breede:  Quartzitic Table Mountain sandstone, Bokkeveld and Malmesbury shales
Lower Breede:  Table Mountain and Witteberg sandstone, Bokkeveld shales, Enon conglomerate, Coastal deposits (Ref 2)
 
    SOILS                                    
  References                                      

Ref 1:   Department of Water Affairs and Forestry, South Africa. 2004. Breede Water Management Area: Internal Strategic Perspective. Prepared by Ninham Shand (Pty) Ltd in association with Jakoet & Associates, Umvoto Africa and Tlou and Matji, on behalf of the Directorate: National Water Resource Planning. DWAF Report No P WMA18/000/00/0304.

Ref 2:   Rivers of the Breede Water Management Area 2011 - State of Rivers Report
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Geology of the Breede River Valley: Worcester to Robertson