Geodetic Study of the 2006–2010 Ground Deformation in La Palma (Canary Islands): Observational Results

La Palma is one of the youngest of the Canary Islands, and historically the most active. The recent activity and unrest in the archipelago, the moderate seismicity observed in 2017 and 2018 and the possibility of catastrophic landslides related to the Cumbre Vieja volcano have made it strongly advis...

Descripción completa

Detalles Bibliográficos
Autores: Escayo, Joaquin, Fernández, José, Prieto, Juan F., Camacho, Antonio G., Palano, Mimmo, Aparicio, Alfredo, Rodríguez Velasco, Gema, Ancochea Soto, Eumenio
Tipo de recurso: artículo
Fecha de publicación:2020
País:España
Institución:Universidad Complutense de Madrid (UCM)
Repositorio:Docta Complutense
Idioma:inglés
OAI Identifier:oai:docta.ucm.es:20.500.14352/6613
Acceso en línea:https://hdl.handle.net/20.500.14352/6613
Access Level:acceso abierto
Palabra clave:550.8:551.21(460.411)
A-DInSAR
GNSS
gravimetry
La Palma
Canary Islands
volcanic unrest
surface deformation
volcano geodetic monitoring
Geodinámica
Petrología
2507 Geofísica
Descripción
Sumario:La Palma is one of the youngest of the Canary Islands, and historically the most active. The recent activity and unrest in the archipelago, the moderate seismicity observed in 2017 and 2018 and the possibility of catastrophic landslides related to the Cumbre Vieja volcano have made it strongly advisable to ensure a realistic knowledge of the background surface deformation on the island. This will then allow any anomalous deformation related to potential volcanic unrest on the island to be detected by monitoring the surface deformation. We describe here the observation results obtained during the 2006–2010 period using geodetic techniques such as Global Navigation Satellite System (GNSS), Advanced Differential Synthetic Aperture Radar Interferometry (A-DInSAR) and microgravimetry. These results show that, although there are no significant associated variations in gravity, there is a clear surface deformation that is spatially and temporally variable. Our results are discussed from the point of view of the unrest and its implications for the definition of an operational geodetic monitoring system for the island