Seismic swarms and earthquake activity b-value related to the September 19, 2021, La Palma volcano eruption in Cumbre Vieja, Canary Islands (Spain)

Mezcua Rodríguez, Julio 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.

Descripción

Título: Seismic swarms and earthquake activity b-value related to the September 19, 2021, La Palma volcano eruption in Cumbre Vieja, Canary Islands (Spain)
Autor/es:
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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Resumen

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.

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ID de Registro: 85955
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...
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Depositado el: 13 Ene 2025 15:29
Ultima Modificación: 13 Ene 2025 15:32