Observations of Deformation
|Region:||Mediterranean and W. Asia|
|Measurement method(s):||InSAR, GPS - campaign|
|Duration of observation:||2002|
|Inferred cause(s) of deformation:||Magmatic, Surface deposits|
|Characteristics of deformation:|
Mattia et al. (2004): The Stromboli volcano erupted suddenly on 28 December 2002 after a 17-year period of typically persistent but moderate eruptive activity, followed two days later by a tsunamigenic landslide on its NW flank (Sciara del Fuoco) felt in the coastal areas of southern Italy.
|Reference(s):||Mattia, M., Rossi, M., Guglielmino, F., Aloisi, M., & Bock, Y. (2004). The shallow plumbing system of Stromboli Island as imaged from 1 Hz instantaneous GPS positions. Geophysical Research Letters, 31(24).|
|Smithsonian Institution Global Volcanism Program|
|Bonaccorso, A., S. Calvari, G. Garfı`, L. Lodato, and D. Patane` (2003),|
Dynamics of the December 2002 flank failure and tsunami at Stromboli
volcano inferred by volcanological and geophysical observations, Geophys.
Res. Lett., 30(18), 1941, doi:10.1029/2003GL017702
|Solaro, G., Castaldo, R., Casu, F., De Luca, C., Marsella, M., Pepe, A., ... & Zeni, G. (2014, May). Insights Into The Dynamics Of Aeolian Volcanic Islands From DInSAR COSMO-SkyMed Observations. In EGU General Assembly Conference Abstracts (Vol. 16, p. 6689).|
|REST API endpoint (JSON):||https://comet.nerc.ac.uk/wp-json/volcanodb/v1/volcano/5264|