The cave system that includes Jameos del Agua and Cueva de los Verdes was formed when La Corona erupted 3,000 years ago. Both sit in the ‘Atlantic Tunnel,’ a section below sea level that runs for 1.6 kms and reaches heights of 50 m. It is now a place of great geological interest.

As the lava flowed over a ravine at some 1200°C, the surface lava slowly cooled, solidifying to form the cave rooves. Meanwhile, hotter lava persisted underneath, flowing towards the sea. When the eruption finally ceased, the bubble-like underground caves were formed as the rooves remained intact.

Driving towards Cueva de los Verdes, you see nothing. The untamed volcanic landscape dominates the horizon, reigned by the majestic summit of La Corona. The signposts are the only indication that you are on the right track.

The birds’ eye view gives a different perspective: the cave entrances appear as great sunken holes, or ‘jameos’in the lava fields, over 20 of them dotting a trail between Corona and the sea. Standing at the entrance to Cueva de los Verdes, you are faced with a dark abyss, luring you into the unknown.

Today, we can fortunately experience this natural wonder at the hand of qualified guides. The cave was first opened for visiting in 1964, following its adaptation by architect Jesús Soto, from Fuerteventura, who later joined forces with César Manrique on several other projects.

Minimal intervention with nature has always been the aim of Lanzarote’s tourist centres, and Cueva de los Verdes is probably the most minimalistic of all. The only evidence of man’s interference are the smooth access paths that lead you through the galleries, music and imaginative lighting effects.