|Measurement method(s):||InSAR, GPS - campaign|
|Duration of observation:||2006 to 2009|
|Inferred cause of deformation:||Uncertain|
|Characteristics of deformation:|
An integrated InSAR and GPS vertical deformation, between 2006 and 2010 map, at Fayal volcano identified a large continuous area of subsidence on the west of Fayal island, on the flank of Capelinhos eruption cone. There was a maximum subsidence range of 10 mm/yr (Catalão et al., 2010). The source of deformation was not studied.
|Reference:||Catalão, J., Nico, G., Hanssen, R., & Catita, C. (2010). Integration of INSAR and GPS for vertical deformation monitoring: a case study in Faial and Pico islands. In Proc. Fringe 2009 Workshop, Frascati, Italy (Vol. 30).|
|Reference:||Smithsonian Institution Global Volcanism Program|
View of Fayal volcano. Source: Smithsonian Institution Global Volcanism Program