This site exposes a representative stratigraphic section of the Baringo Basin, with evidence of volcanosedimentary sequences.
A steep volcanic pillar formed by erosion of the surrounding softer rocks.
An isolated volcanic plug standing as a natural monument of past volcanic activity.
A tall volcanic rock formed when resistant magma remained after the surrounding rocks eroded.
The site features an abandoned borehole. Its construction was halted following the release of non-combustible gases from the vent.
The Chepkokon Mushroom Rock City displays a well-preserved stratigraphic succession that records rift-related magmatic and sedimentary processes.
