Articles | Volume 8, issue 3
https://doi.org/10.5194/se-8-697-2017
https://doi.org/10.5194/se-8-697-2017
Research article
 | 
23 Jun 2017
Research article |  | 23 Jun 2017

Dynamics and style transition of a moderate, Vulcanian-driven eruption at Tungurahua (Ecuador) in February 2014: pyroclastic deposits and hazard considerations

Jorge Eduardo Romero, Guilhem Amin Douillet, Silvia Vallejo Vargas, Jorge Bustillos, Liliana Troncoso, Juan Díaz Alvarado, and Patricio Ramón

Viewed

Total article views: 3,409 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,969 1,192 248 3,409 160 157
  • HTML: 1,969
  • PDF: 1,192
  • XML: 248
  • Total: 3,409
  • BibTeX: 160
  • EndNote: 157
Views and downloads (calculated since 14 Dec 2016)
Cumulative views and downloads (calculated since 14 Dec 2016)

Viewed (geographical distribution)

Total article views: 3,409 (including HTML, PDF, and XML) Thereof 3,124 with geography defined and 285 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Discussed (preprint)

Latest update: 05 Nov 2024
Download
Short summary
The 1 February 2014 eruption of the Tungurahua volcano (Ecuador) was the second largest one since the re-awakening in 1999. The eruption showed precursory signs only 48 h before the eruption. The main explosions produced a 13 km eruptive column and pyroclastic density currents that reached the base of the volcano. Here we document the deposits related to the eruption and infer eruption mechanisms and transport processes.