Solid Earth
Solid Earth
SE
Articles | Volume 14, issue 1
Articles | Volume 14, issue 1
https://doi.org/10.5194/se-14-69-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-14-69-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 14, issue 1
Research article
 | Highlight paper
 | 
23 Jan 2023
Research article | Highlight paper |  | 23 Jan 2023

Anatomy of a high-silica eruption as observed by a local seismic network: the June 2011 Puyehue–Cordón Caulle event (southern Andes, Chile)

Daniel Basualto, Andrés Tassara, Jonathan Lazo-Gil, Luis Franco-Marin, Carlos Cardona, Juan San Martín, Fernando Gil-Cruz, Marcela Calabi-Floddy, and Cristian Farías

Viewed

Total article views: 1,891 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,432 408 51 1,891 130 29 27
  • HTML: 1,432
  • PDF: 408
  • XML: 51
  • Total: 1,891
  • Supplement: 130
  • BibTeX: 29
  • EndNote: 27
Views and downloads (calculated since 01 Jun 2022)
Cumulative views and downloads (calculated since 01 Jun 2022)

Viewed (geographical distribution)

Total article views: 1,891 (including HTML, PDF, and XML) Thereof 1,801 with geography defined and 90 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 18 Apr 2024
Download
Executive editor
The paper represents a very detailed study of the geophysical precursors recorded before and during a major recent explosive eruption. Moreover, the results permit to partly validate and discuss recent models of volcano unrest and have large applications for the monitoring of hazardous volcanoes worldwide.
Read more
Short summary
Infrequent eruptions of acidic magma are one of the most dangerous natural phenomena, but almost none of them have been witnessed by modern science. We present the first systematic characterization of seismicity recorded near an erupting acidic volcano (Cordón Caulle 2011). We define different phases of unrest and eruption, which combined with previous findings allows us to discuss the main processes associated with this type of violent eruption, with implications for their volcanic hazard.
Read more