Observations of Deformation
| Volcano number: | 382010 |
|---|---|
| Region: | Atlantic Ocean |
| Country: | Portugal |
| Geodetic measurements? | Yes |
| Deformation observation? | Yes |
| Measurement method(s): | InSAR, GPS - campaign |
| Duration of observation: | 2006 to 2009 |
| Inferred cause(s) 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(s): | 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). |
| Smithsonian Institution Global Volcanism Program http://www.volcano.si.edu/volcano.cfm?vn=382010 | |
| Location: | 38.6, -28.73 |
| REST API endpoint (JSON): | https://comet.nerc.ac.uk/wp-json/volcanodb/v1/volcano/5216 |
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