Lanzarote, Spain


Lanzarote is located 11 km (7 mi) north-east of Fuerteventura and just over 1 km (0.62 mi) from Graciosa. The dimensions of the island are 60 km (37 mi) from north to south and 25 km (16 mi) from west to east. Lanzarote has 213 km (132 mi) of coastline, of which 10 km (6 mi) are sand, 16.5 km (10 mi) are beach, and the remainder is rocky. Its landscape includes the mountain ranges of Famara (671 meters (2,201 ft)) in the north and Ajaches (608 m) to the south. South of the Famara massif is the El Jable desert which separates Famara and Montañas del Fuego. The highest peak is Peñas del Chache rising to 670 meters (2,198 ft) above sea level. The "Tunnel of Atlantis," the largest underwater volcanic tunnel in the world, is part of the Cueva de los Verdes lava tube.

Lanzarote is the easternmost island of the Canary Islands and has a volcanic origin. It was born through fiery eruptions and has solidified lava streams as well as extravagant rock formations. The island emerged about 15 million years ago as product of the Canary hotspot. Alfred Wegener's study of the island whilst visiting in 1912 showed how it fitted in with his theory of continental drift. The island, along with others, emerged after the breakup of the African and the American continental plates. The greatest recorded eruptions occurred between 1730 and 1736 in the area now designated Timanfaya National Park.


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