|Region:||Mexico and Central America|
|Measurement method(s):||No measurements|
|Duration of observation:|
|Inferred cause of deformation:|
|Characteristics of deformation:|
Previous InSAR studies of Central American volcanoes did not cover Tajumulco due to it’s position at the end of the Central American Volcanic Arc (Ebmeier et al., 2013).
|Reference:||Ebmeier, S. K., J. Biggs, T. A. Mather and F. Amelung (2013), Applicability of InSAR to tropical volcanoes: insights from Central America, Geological Society of London Special Publications, 380, Remote-sensing of volcanoes and volcanic processes: Integrating observation and modelling, doi:10.1144/SP380.2.|
View of Tajumulco from the north-northwest. Photo: Bill Rose, 1986 (Michigan Technological University).