| KEURBOOMS RIVER: Topography, geology and soils |
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eWISA Home | KEURBOOMS: MAIN INDEX | ALPHABETICAL LIST OF RIVERS | ||||||||||||||||||||||
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Map of the KEURBOOMS River |
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| TOPOGRAPHY | |||||||||||||||||||||||
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One
of the major features of the region is the Jurassic, west-east trending
Cape Fold Belt and in particular the southern orographic line, which
includes the Outeniqua, Langkloof and |
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The southern
boundary of the Keurbooms catchment is situated on the coast. The
mountains to the north are rugged and barely accessible (Ref. 12).
The main Outeniqua mountain range, elevation >1200 m, runs
east-west and the south-facing slopes are significantly moister than the
north-facing slopes. The coastal section includes a broad elevated
coastal plateau (150–250 m) with deeply incised river valleys. |
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| GEOLOGY | |||||||||||||||||||||||
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The
drainage basin of the |
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| SOILS | |||||||||||||||||||||||
| The Table Mountain Group weathers to acid, well-drained soil. Fluvial sand forms only a small part of the estuarine sediment input (Ref. 2). | |||||||||||||||||||||||
| Apart from the presence of swelling clays in certain areas, large areas are covered by sandy soil and drift sand (Ref. 9). | |||||||||||||||||||||||
| References | |||||||||||||||||||||||
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Ref 1: Duvenhage,
I.R. and Morant, P.D. (1984). Estuaries of the Cape Part II: Synopses of
available information on individual systems.
Report No. 31 Keurbooms/Bitou System (CMS 19) Piesang (CMS18).
CSIR Research Report 430. 64pp.
Ref 2:
Reddering,
J.S.V. (1981). The
sedimentology of the Keurbooms Estuary.
M.Sc. thesis. |
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