Suspension bridge between pinnacles in the Tsingy de Bemaraha

Karst landscapes

Where the continent's caves are, what rocks they are in and how they formed.

3 guides
Overview

A continent with scattered karst

Three pages on the geology behind the caves.

Much of Africa is made of very old crystalline rock that does not form caves. Limestone and dolomite occur in separate regions, and the caves are concentrated there.

The pages in this section explain how limestone caves form, where the main cave regions are, and how sinkhole lakes and volcanic caves differ from ordinary karst.

2.6bn

years: approximate age of the dolomite at Sterkfontein

100m

height of the tallest pinnacles in the Tsingy de Bemaraha

8

countries represented on this guide

See the sites

Ten caves and karst sites are described on their own pages.

All caves Plan your visit