The Pitcairn Islands form the southeasternmost extension of the geological archipelago of the Tuamotus of French Polynesia, and consist of four islands: Pitcairn Island, Oeno Island (atoll with five islets, one of which is Sandy Island), Henderson Island and Ducie Island (atoll with four islets).
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Geography of the Pitcairn Islands
03/08/2019
The only permanently inhabited island, Pitcairn, is accessible only by boat through Bounty Bay.
Henderson Island, covering about 86% of the territory's total land area and supporting a rich variety of animals in its nearly inaccessible interior, is also capable of supporting a small human population, but access is difficult, owing to its outer shores' being steep limestone cliffs made of sharp coral.
The Pitcairn Islands were formed by a centre of upwelling magma called the Pitcairn hotspot.
The other islands are at a distance of more than 100 km (60 mi) and are not habitable.
Henderson Island, covering about 86% of the territory's total land area and supporting a rich variety of animals in its nearly inaccessible interior, is also capable of supporting a small human population, but access is difficult, owing to its outer shores' being steep limestone cliffs made of sharp coral.
The Pitcairn Islands were formed by a centre of upwelling magma called the Pitcairn hotspot.
The other islands are at a distance of more than 100 km (60 mi) and are not habitable.