ABSTRACT

All the Azorean islands are of volcanic origin and correspond to the elevations of the ocean floor due to the accumulation of volcanic products. The archipelago is located in a very active seismic and volcanic area that corresponds to an area where the American, Eurasian and African lithospheric plates meet (Gaspar et al., 2007; Costa et al., 2008), and this translates in the existence of important fault systems (Fig. 1).