|Duration of observation:||2006-2008|
|Inferred cause of deformation:|
|Characteristics of deformation:|
No deformation was detected at Qualibou during an ALOS survey of Latin American volcanoes (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 from the north, overlooking the town of Soufrière, of Petit Piton (right) and Gros Piton (left), two lava domes associated with the Qualibou caldera. Photo: David Arnold, 2015 (University of Bristol).