SABIE RIVER: Hydrology and geohydrology

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Map of the SABIE River

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HYDROLOGY
"Mean annual runoff in the Sabie-Sand Catchment is approximately 762 million cubic metres. Flows in the Sabie River peak in summer, and low flows are experienced at the end of the winter dry season, although no-flow conditions have never been recorded."(www.csir.co.za/rhp/state_of_rivers/state_of_crocsabieolif_01/sabie_eco.html)
"This ecoregion covers the upper section of the Drakensberg Escarpment, with altitudes between 1 000 and 2 000 m above mean sea level, and high mountainous relief. As a consequence of the range in altitude and relief, there is a large variation in rainfall (600-1 200 mm per year) and mean annual temperature (10-18°C)." (www.csir.co.za/rhp/state_of_rivers/state_of_crocsabieolif_01/sabie_eco.html)
    GEOHYDROLOGY                                    
The headwaters of the Sabie River and its tributaries (the Sand, Marite, Mutlumuvi, Motitsi and Mac Mac Rivers) arise in the upper parts of the escarpment. These rivers are cold mountain streams, narrow with moderate to steep gradients, and hence fast flowing. Waterfalls are common, and rocky pools and rapids abound." (www.csir.co.za/rhp/state_of_rivers/state_of_crocsabieolif_01/sabie_eco.html)
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