|Region:||Mexico and Central America|
|Measurement method(s):||InSAR, GPS - continuous|
|Duration of observation:||2007-2010 (InSAR), 2010-2013 (continuous GPS)|
|Inferred cause of deformation:|
|Characteristics of deformation:|
No deformation was detected at Telica (detection threshold 1.8 cm/yr) during an ALOS survey of Central American volcanoes (Ebmeier et al., 2013).
No transient deformation was observed in a 10 station cGPS network during eruptions at Telica during March-June 2011 (Geirsson et al., 2014)
|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.|
|Reference:||Halldor Geirsson, Mel Rodgers, Peter LaFemina, Molly Witter, Diana Roman, Angelica Muñoz, Virginia Tenorio, Julio Alvarez, Vladimir Conde Jacobo, Daniel Nilsson, Bo Galle, Maureen D. Feineman, Tanya Furman, Allan Morales, Multidisciplinary observations of the 2011 explosive eruption of Telica volcano, Nicaragua: Implications for the dynamics of low-explosivity ash eruptions, Journal of Volcanology and Geothermal Research, Volume 271, 1 February 2014, Pages 55-69, ISSN 0377-0273, http://dx.doi.org/10.1016/j.jvolgeores.2013.11.009.|
Aerial view of Telica volcano from the north. Photo: Jaime Incer, 1991.