Image by Carol Howes
The source of all the rivers of Zandvlei rise in the Cape Peninsula Mountains. The Diep River has the longest course, approximately 15 kilometers from source to Zandvlei. These rivers are the life blood of Zandvlei and have to be carefully monitored to make sure of the sustainability of Zandvlei.
Zandvlei is an estuary, which has a delicate, cyclic and seasonal balance of sea to fresh water mix. This mix determines its life supporting capabilities.
Developments along the water courses have impacted negatively, in that excessive nutrients (fertilisers) and sediments (top soil erosion) are being deposited in Zandvlei in the high run off periods.
Also seriously affecting the rivers is lack of regular road gutter and storm water drain sump cleaning. The silt ends up in the storm water drains which feeds into the rivers and then into Zandvlei. If damming and water extraction of these rivers is not carefully controlled, the inflow to Zandvlei can be seriously affected.

Prinskasteel River in May 2010.
photograph by Greg Morgan

Prinskasteel River in May 2007.
photograph by Greg Morgan
Map of the Zandvlei catchment rivers and boundaries
Zandvlei Catchment Management boundaries, November 2015.
Catchment Rivers
Sand River

This is the confluence of the Sand River into the Langevlei River, in a flood plain, South of Coniston Park.
Langevlei River

The old litter trap in the Langevlei canal which were moved about 100 meters North upstream, to a new location. The moving of the litter trap is part of the Wetland development project.
Keyser River



Westlake River



Grootboschkloof River

Prinskasteel River

Spaanschemat River


