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There are no activity reports for Fuerteventura.
Available Weekly Reports
There are no Weekly Reports available for Fuerteventura.
There are no Holocene eruptions known for Fuerteventura. If this volcano has had large eruptions prior to 10,000 years ago, information might be found in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).
The following references are the sources used for data regarding this volcano. References are linked directly to our volcano data file. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title. Additional discussion of data sources can be found under Volcano Data Criteria.
Arana V, Carracedo J C, 1979. Los Volcanes de las Islas Canarias. II. Lanzarote-Fuerteventura. Madrid: Rueda, 176 p.
Fuster J M, Cendrero A, Gastesi P, Ibarrola E, Lopez-Ruiz J, 1968. Geologia y Volcanologia de las Islas Canarias - Fuerteventura. Madrid: Inst "Lucas Mallada", 239 p.
Mitchell-Thome R C, 1976. Geology of the Middle Atlantic Islands. Berlin: Gebruder Borntraeger, 382 p.
Neumann van Padang M, Richards A F, Machado F, Bravo T, Baker P E, Le Maitre R W, 1967. Atlantic Ocean. Catalog of Active Volcanoes of the World and Solfatara Fields, Rome: IAVCEI, 21: 1-128.
Schmincke H-U, Sumita M, 2010. Geological evolution of the Canary Islands. Koblenz: Gorres-Verlag: 188 p.
Pleistocene and Holocene cinder cones and lava flows cover large portions of elongated Fuerteventura Island at the SE end of the Canary Islands. The youngest lavas are found at the northern and central portions of the arid, sparsely vegetated island. Malpais de la Arena, the Northern Malpais, and the Lobos Island areas at the northern tip of Fuerteventura are the sites of broad fields of youthful cinder cones and lava flows. The Malpais Chico, Malpais Grande, and Malpais de Jacomar areas on the south-central part of the island represent smaller zones of youthful volcanism, as do the volcanoes of Pajara, which were constructed on the older plutonic massif west of the axis of the island. No historical eruptions have occurred on Fuerteventura. although the very youthful appearance of lava flow surfaces in the central part of the island suggests a late-Holocene or prehistoric age.