Recent structural evolution of the Cumbre Vieja volcano, La Palma, Canary Islands: volcanic rift zone reconfiguration as a precursor to volcano flank instability?

Author:

Day S.J,Carracedo J.C,Guillou H,Gravestock P

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference46 articles.

1. Afonso, A., 1974. Geological sketch and historic volcanoes in La Palma, Canary Islands. Estudios Geologicos, Teneguia Volume, 7–13.

2. Constructive and destructive episodes in the building of a young oceanic island, La Palma, Canary Islands, and the genesis of the Caldera de Taburiente;Ancochea;J. Volcanol. Geotherm. Res.,1994

3. The dynamics of the formation of cone sheets, ring dykes and cauldron subsidence;Anderson;Proc. R. Soc. Edinburgh,1935

4. Bonelli Rubio, J.M., 1950. Contribucion al estudio de la erupcion del Nambroque o San Juan (isla de La Palma), (Contribution to the study of the eruption of Nambroque or San Juan (island of La Palma). Madrid, Instituto Geografico y Catastral, 25 pp.

5. The Canary islands: an example of structural control on the growth of large oceanic-island volcanoes;Carracedo;J. Volcanol. Geotherm. Res.,1994

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