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ORCID: https://orcid.org/0000-0001-9299-0088 and Rueda Núñez, Juan José
ORCID: https://orcid.org/0000-0003-2350-4423
(2023).
Seismic swarms and earthquake activity b-value related to the September 19, 2021, La Palma volcano eruption in Cumbre Vieja, Canary Islands (Spain).
"Bulletin of Volcanology", v. 85
(n. 32);
ISSN 02588900.
https://doi.org/10.1007/s00445-023-01646-z.
| Título: | Seismic swarms and earthquake activity b-value related to the September 19, 2021, La Palma volcano eruption in Cumbre Vieja, Canary Islands (Spain) |
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| Autor/es: |
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| Tipo de Documento: | Artículo |
| Título de Revista/Publicación: | Bulletin of Volcanology |
| Fecha: | 25 Abril 2023 |
| ISSN: | 02588900 |
| Volumen: | 85 |
| Número: | 32 |
| Materias: | |
| Palabras Clave Informales: | Swarm seismicity, Magma ascen, Gutenberg–Richter b parameter |
| Escuela: | E.T.S.I. en Topografía, Geodesia y Cartografía (UPM) |
| Departamento: | Ingeniería Topográfica y Cartografía |
| Licencias Creative Commons: | Reconocimiento |
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The recent eruption of the Cumbre Vieja Volcanic Ridge in La Palma started on September 19, 2021, after a series of seismic swarms and lasted 85 days. Seismic swarms showed a large variability but could be grouped in two categories: long-term swarms located at subcrustal depth, showing b-values close to 2.2 and low rates (from 4.1 to 56 events/hour) and short-term swarms located at very shallow depths, showing moderate b-values [0.9, 1.6] and high rates (from 58 to 460 events/hour). Magma ascent velocity within the 0–10 km depth range varied between 0.03 and 0.21 km/h. Spatial and temporal characterization of the b-values for the entire magmatic process during the selected study period also indicated three distinct dynamics during a preparation phase starting from at least October 2017–August 2021, the eruptive phase from September 2021–December 2021 and a post-eruption process from the end of the eruption in December 2021–May 2022. These stages with clearly different values reflect two scenarios: one corresponding to the time before the eruption with magma ascending from a 39-km depth to the surface, and a second stage corresponding to the eruption itself which includes two seismicity concentrations within the 30–40 km depth interval and a shallow concentration from 0–20 km, corresponding to the crustal reservoir and movement towards the surface.
| ID de Registro: | 85955 |
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| Identificador DC: | https://oa.upm.es/85955/ |
| Identificador OAI: | oai:oa.upm.es:85955 |
| URL Portal Científico: | https://portalcientifico.upm.es/es/ipublic/item/10041750 |
| Identificador DOI: | 10.1007/s00445-023-01646-z |
| URL Oficial: | https://link.springer.com/article/10.1007/s00445-0... |
| Depositado por: | Portal Científico UPM |
| Depositado el: | 13 Ene 2025 15:29 |
| Ultima Modificación: | 13 Ene 2025 15:32 |
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