Why study volcanology with us in the Canary Islands?
The Canary Island archipelago consists of seven major islands. La Palma and El Hierro are the youngest in the southwest; Lanzarote and Fuerteventura are the oldest in the northeast. Only four of the islands—Tenerife, La Palma, El Hierro, and Lanzarote—have experienced volcanic eruptions in the last 500 years.
Tenerife, located in the central-western part of the archipelago, is the largest island and hosts the third-largest volcanic structure on Earth. It has seen numerous highly explosive eruptions, which form calderas and pyroclastic density currents, as well as effusive mafic eruptions at its rift zones.
The magmatic plumbing system of the Canary Islands features diverse geochemistry, leading to a variety of volcanic phenomena, including both explosive and effusive eruptions, and producing felsic and mafic volcanic products. This diversity results in a range of volcanic features such as lava flows, lava deltas, lava tubes, ignimbrites, calderas, stratovolcanoes, shield volcanoes, and pyroclastic cones. VolcanoCamp leverages this geological diversity to provide students from around the world with an intensive, hands-on volcanology course in the Canary Islands.