| Volcano number: | 351050 |
|---|---|
| Region: | South America |
| Country: | Colombia |
| Geodetic measurements? | Yes |
| Deformation observation? | No |
| Measurement method(s): | InSAR |
| Duration of observation: | Unknown |
| Inferred cause of deformation: | [] |
| Characteristics of deformation: |
No deformation was detected at Nevado del Huila between 2006 and 2009 during ALOS surveys of Latin American volcanoes (Fournier et al., 2010, Parks et al., 2011). |
| References: | '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.', 'Parks, M. M., J. Biggs, T. A. Mather, D. M. Pyle, F. Amelung, M. L. Monsalve, and L. Narváez Medina (2011), Co-eruptive subsidence at Galeras identified during an InSAR survey of Colombian volcanoes (2006–2009), Journal of Volcanology and Geothermal Research 202, no. 3, 228-240, doi:10.1016/j.jvolgeores.2011.02.007' |
| Location: | -76.03, 2.93 |
