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Geography of the British Virgin Islands

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  • 3 chapters

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Through Archipelago, Atlantic Ocean and Tectonics

Terrain

The majority of the islands are steep and hilly due to their volcanic origin. The lowest point of the island chain is the Caribbean Sea while the highest point is Mount Sage at 521 metres (1,709 ft) above sea level and there are 80 kilometres (50 mi) of coastline. Other than Anegada, the islands are composed of pyroclastic rock and mixed deposits of diorite and tonalite Anegada is geologically distinct, being composed of carbonate reef deposits. The entire archipelago, together with Puerto Rico to the west, is the above-water high points on an underwater ridge that was once a continuous land mass during the Pleistocene epoch. This bank formed from tectonic forces at the boundary where the Caribbean Plate collides with the North American Plate. In the British Virgin Islands forest cover is around 24% of the total land area, equivalent to 3,620 hectares (ha) of forest in 2020, down from 3,710 hectares (ha) in 1990.

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