The Cumbre Vieja (Spanish pronunciation: ['kumb?e 'ßjexa]; meaning Old Summit) is an active volcanic ridge on the island of La Palma in the Canary Islands, Spain.
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“There is continuous seismicity between Gran Canaria and Tenerife. We have evidence of it since earthquakes began to be documented in the Canary Islands in the 1950s, when the first seismic station was installed, and then, with the expansion of the network during the 70s”.
Eruptions on La Palma can last from a few weeks to several months. “The only way to know is to know the total volume of eruptible magma under Cumbre Vieja,” says Pablo J. González, a physical volcanologist at the Spanish National Research Council on Tenerife.
The Canary Islands were created by a series of volcanic eruptions millions of years ago. The oldest of these is Fuerteventura, which is thought to be over 20 million years old, followed by Lanzarote, Gran Canaria, Tenerife, La Gomera, La Palma and El Hierro, respectively.
Although politically they are part of Spain, the Canary Islands are closer to Africa than they are to Europe and so geographically they are part of the African continent. Fuerteventura is the closest island to Africa, situated at only a 100 km distance from the coast of Morocco.