Articles | Volume 20, issue 12
https://doi.org/10.5194/nhess-20-3627-2020
https://doi.org/10.5194/nhess-20-3627-2020
Research article
 | 
23 Dec 2020
Research article |  | 23 Dec 2020

Remote monitoring of seismic swarms and the August 2016 seismic crisis of Brava, Cabo Verde, using array methods

Carola Leva, Georg Rümpker, and Ingo Wölbern

Viewed

Total article views: 1,680 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,133 478 69 1,680 255 59 50
  • HTML: 1,133
  • PDF: 478
  • XML: 69
  • Total: 1,680
  • Supplement: 255
  • BibTeX: 59
  • EndNote: 50
Views and downloads (calculated since 03 Aug 2020)
Cumulative views and downloads (calculated since 03 Aug 2020)

Viewed (geographical distribution)

Total article views: 1,680 (including HTML, PDF, and XML) Thereof 1,493 with geography defined and 187 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 20 Nov 2024
Download
Short summary
Often, an abrupt increase in shallow seismicity at volcanoes is seen as an indicator for magmatic intrusions into the upper crust. If no eruption occurs and the seismic activity stops, this is called a failed eruption. Here, we report a failed eruption of Brava, Cabo Verde, in August 2016. We remotely monitored the seismicity of Brava with a seismic array, operating from October 2015 to December 2016. Other episodes with increased seismicity around the island were also observed during the study.
Altmetrics
Final-revised paper
Preprint