PIENAARS RIVER: Topography, geology and soils

eWISA Home  |  PIENAARS: MAIN INDEX  ALPHABETICAL LIST OF RIVERS
                             
 

Map of the PIENAARS River

E-mail us                    
TOPOGRAPHY
    GEOLOGY                                    
Headwaters of the Pienaars River are located in an area underlain by formations of acid and intermediate lavas, arenaceous and argillaceous strata, and basic and acidic rocks of the Bushveld Complex and the granites of the Waterberg Formation. (Ref 2)
    SOILS                                    

Soils in the sub-catchment can be divided into four main groups:

  • Moderate to deep sandy loam soils on flat and undulating terrain overlying dolomite, limestone and sandstones in the upper reaches of the catchment;

  • Moderate to deep clay loam soils over much of the middle portions of the sub-catchment (located away from the river channels), overlying the more porous unconsolidated sedimentary material; and

  • Moderately shallow to moderately deep, clayey loam to clay-rich, fine-grained soils over most of the lower reaches of the sub-catchment.  (Ref 2)

Dolomitic rock is also found at the confluence of the Tolwane and Pienaars rivers as well as the confluence of the Pienaars and Crocodile rivers in the Apies/Pienaars sub-catchment. (www.csir.co.za/rhp/state_of_rivers/crocwestmarico_05/crocwestmarico_05_A3.pdf
0003116.JPG (63901 bytes) 0003117.JPG (63450 bytes) 0003118.JPG (78014 bytes) 0003119.JPG (63734 bytes) 0003123.JPG (76266 bytes)
0003123.JPG (76266 bytes) 0003124.JPG (48874 bytes) 0003126.JPG (59597 bytes) 0002865.JPG (64129 bytes)
  References                                      

Ref 2:  www.mining.wits.ac.za/FinancialReportSection4.doc
  Useful links