Reference Edition
Geography Atlas
Waterfall Record

Tugela Falls

Tugela Falls descends from the Drakensberg escarpment, where highland runoff drops over steep cliff faces in a multi-stage waterfall system.

Drakensberg escarpment setting

The falls are tied to the abrupt plateau edge of the Drakensberg. Relief, cliff structure, and seasonal water supply control the waterfall's visible form.

Seasonal flow and cliff descent

Flow varies with rainfall and highland runoff. The long descent emphasizes escarpment height more than river width.

Edge

Escarpment cliff

The plateau margin creates the vertical drop.

Water

Seasonal runoff

Highland rainfall controls discharge.

Terrain

Southern African highlands

The falls belong to a larger mountain-edge system.