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3. ECOLOGICAL CHARACTERISTICS AND FUNCTIONING OF<br />

THE ESTUARY<br />

3.1 Mouth dynamics, hydrology and channel shape<br />

The Uilkraals Estuary has been classified as a temporarily open-closed estuary (Whitfield 2000),<br />

and is a mixed (in terms of salinity), blackwater system (van Niekerk unpubl. data). When<br />

functioning naturally, the estuary has tidal exchange and a high frequency of connection to the<br />

sea, similar to the Palmiet and Kleinmond estuaries, but is in a more advanced stage of<br />

progressive infilling and reduction of the tidal prism (Harrison et al. 1995a). The road bridge,<br />

which was constructed in 1973, is approximately 220 m long and crosses the river<br />

approximately 800 m from the mouth (Figure 9 and Figure 10). It is supported on the eastern<br />

side by a high embankment of rubble spanning almost two-thirds of the original high tide river<br />

width (Gaigher 1984). The remaining 100 m are supported by concrete pylons, effectively<br />

halving the width of the estuary there and concentrating the river flow against the western<br />

bank (Heydorn & Bickerton 1982). In 1978 a 150 m long rubble and rock embankment was<br />

built on the beach in front of the beach facing bungalows, forcing the estuary mouth<br />

eastwards, away from the caravan park (Heydorn & Bickerton 1982). However, the<br />

embankment was quickly eroded by wave and tidal action and a shallow, stagnant pool of<br />

water and a series of sand dunes formed on the beach in front of the bungalows (Figure 9).<br />

In the past the estuary mouth opened over a beach with a relatively flat profile and the open<br />

mouth status was probably maintained by strong tidal currents (Harrison 2004). Tidal currents<br />

play a major role in maintaining a connection with the sea in cool and warm-temperate<br />

estuaries (unlike subtropical estuaries, where river flow is the major factor; Cooper et al. 1999,<br />

Cooper 2001). Seasonal closure and migration of the estuary occurs due to strong seasonal<br />

variations of river flow and wave climate where limited river flow allows the formation of a<br />

sand bar across the estuary mouth.<br />

Uilkraals Estuary Situation Assessment<br />

18<br />

<strong>Anchor</strong> <strong>Environmental</strong>

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