The Cueva Canal de Pico Partido, an ancient lava flow and tunnel, in Timanfaya National Park, Lanzarote, Canary Islands. Lanzarote has a volcanic orig
The Cueva Canal de Pico Partido, an ancient lava flow and tunnel, in Timanfaya National Park, Lanzarote, Canary Islands. Lanzarote has a volcanic origin, emerging about 15 million years ago after the break-up of the African and the American continental plates. Volcanic eruptions were recorded between 1730 and 1736 in the area now designated Timanfaya National Park.
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Photo credit: © BOB GIBBONS/SCIENCE PHOTO LIBRARY / Alamy / Afripics
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