Nevados de Chillan

Observations of Deformation

Volcano number:357079
Geodetic measurements?Yes
Deformation observation?No
Measurement method(s):InSAR, Seismic Data
Duration of observation:2006-2008 (InSAR) December 2011 to April 2012 (Seismic)
Inferred cause(s) of deformation:Faulting/tectonics
Characteristics of deformation:

No deformation was detected at Nevados de Chillan during a regional ALOS InSAR survey of Southern Andean Volcanoes (Fournier et al., 2010).
Seismicity characterized by numerous volcano tectonic events and tremor episodes occurring within the volcanic complex after Maule 2012 Earthquake (Mw 6.1 in January 2012, and Mw 7.1 in April 2012)(Farías et al., 2014).

Reference(s):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.
Farías, C., Lupi, M., Fuchs, F., & Miller, S. A. (2014). Seismic activity of the Nevados de Chillán volcanic complex after the 2010 Mw8. 8 Maule, Chile, earthquake. Journal of Volcanology and Geothermal Research, 283, 116-126.
Location:-36.863, -71.377
REST API endpoint (JSON):

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