Waterfall Record

Victoria Falls

Victoria Falls is a major Zambezi River waterfall where plateau flow drops into a fracture-controlled chasm and then enters a series of narrow gorges.

Why This Record Matters

A plateau-edge waterfall and gorge system

Victoria Falls connects southern African plateau drainage, basalt structure, spray-zone microclimate, and downstream gorge incision in one record.

TypePlateau-edge waterfall

A broad river drop across resistant bedrock.

RiverZambezi River

The falls sit within the middle Zambezi system.

ProcessFracture-guided gorge

Jointed basalt helps focus erosion and retreat.

Linked BasinSouthern African plateau

Seasonal flow comes from a broad interior basin.

Overview

What Victoria Falls is

Victoria Falls is a large waterfall on the Zambezi River, set within a plateau landscape where water crosses a bedrock edge and drops into a deep chasm.

The falls are best understood as a waterfall-gorge system rather than only a brink line.

Gorge

Basalt fractures and retreating edges

Fractures in basalt guide the waterfall edge and the downstream gorge pattern. As water exploits these weaknesses, plunge pools and gorge segments preserve the history of retreat.

Brink

Wide river edge

The Zambezi crosses a broad rock lip before dropping.

Spray

Local moisture zone

Mist and spray shape the immediate waterfall margin.

Gorge

Incised downstream route

The river exits through narrow bedrock gorges.

Basin

Zambezi flow context

The waterfall depends on seasonal Zambezi discharge gathered from a large upstream basin. River volume changes the visible form of the falls through the year.