|Duration of observation:||2006|
|Inferred cause of deformation:|
|Characteristics of deformation:|
No deformation was detected at Saba during an 2006-2008 ALOS survey of Latin America, however due to limited data, interferograms could only be made spanning 3 months in 2006 (Fournier et al., 2010).
|Reference:||Fournier, T. J., M. E. Pritchard, and S. N. Riddick (2010), Duration, magnitude, and frequency of subaerial volcano deformation events: New results from Latin America using InSAR and a global synthesis, Geochem. Geophys. Geosyst., 11, Q01003, doi:10.1029/2009GC002558.|
View of the summit of Saba from the northeast. Photo: John Shepherd, 2000 (Seismic Research Unit, University of West Indies).