|Region:||Mexico and Central America|
|Duration of observation:||2007-2010|
|Inferred cause of deformation:|
|Characteristics of deformation:|
No deformation was detected at Almolonga (detection threshold 0.8 cm/yr) during an ALOS survey of Central American volcanoes (Ebmeier et al., 2013).
|Reference:||Ebmeier, S. K., J. Biggs, T. A. Mather, and F. Amelung (2013), On the lack of InSAR observations of magmatic deformation at Central American volcanoes, J. Geophys. Res. Solid Earth, 118, 2571–2585, doi:10.1002/jgrb.50195.|
View, from the east, of the Cerro Quernado lava dome complex (rounded hills in the centre of the photo, to the right of the Santa Maria stratovolcano), part of Almolonga volcanic field. Photo: Lee Siebert, 1988, (Smithsonian Institution).