Piton de la Ravine des Cafres

Piton de la Ravine des Cafres is a mountain summit in Réunion reaching approximately 1200 meters in elevation. The slopes reveal multiple layers of rock and exposed geological materials that formed through volcanic processes over long periods.

The mountain formed through multiple volcanic episodes millions of years ago that shaped the island of Réunion. These ancient geological events remain visible in the rock layers and composition of the peak today.

The mountain holds significance for people living on Réunion, serving as a landmark that connects them to the island's natural landscape and identity. Visitors notice how locals relate to the peak as part of their everyday geography and regional pride.

The summit is reached via marked hiking trails that provide clear routes up the mountain. Plan your visit for early morning to benefit from better weather conditions and clearer views from the top.

From the summit, hikers can observe the distinct rock layers that record the volcanic history written into the mountainside. Each layer represents a different phase of the island's formation, creating a natural record visible to visitors.