Makatea

Makatea is a raised coral island in French Polynesia within the administrative subdivision of the Tuamotu‑Gambier group. Unlike low atolls, Makatea rises steeply from the ocean to an elevated limestone plateau ringed by cliffs.

The island’s geology and raised‑atoll form produced phosphate deposits that were exploited commercially during the 20th century, leaving mining features and altered landscapes. Today the island retains steep coastal cliffs, interior karst features and small settlements.

Access is by air or sea from larger population centres in French Polynesia, and services on the island are limited compared with the Society Islands. The island’s topography and remoteness make it distinct among the Tuamotu‑Gambier islands.

Makatea lies in the central South Pacific as part of French Polynesia’s overseas territory and is administered within the Tuamotu‑Gambier subdivision.

• Raised atoll morphology: a raised coral island with steep limestone cliffs that distinguishes it from typical low atolls in the region.
• Phosphate mining history: site of historical phosphate extraction which shaped the island’s economy and landscape in the 20th century.

• Makatea is a small raised coral island with limited accommodation and transport - arrange your inter-island flight or boat connection and any on-island transfers well in advance because services are infrequent.
• The island has visible remnants of historic phosphate-mining infrastructure and rugged limestone cliffs and caves; if you want to explore these safely and respectfully, hire a local guide rather than attempting solo explorations in remote areas.
• Bring sufficient cash and confirm lodging/meals ahead of arrival: services can be basic and not all amenities are available on short notice.