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Shallow magmatic intrusion evolution below La Palma before and during the 2021 eruption
José Fernández1, Joaquin Escayo2, Antonio G Camacho2
1Instituto de Geociencias (CSIC, UCM). Calle del Doctor Severo Ochoa, nº 7, Ciudad Universitaria, 28040, Madrid, Spain. jft@mat.ucm.es.
The 2021 La Palma eruption was preceded by shallow magma accumulation. Advanced InSAR analysis revealed low-density, fractured rock zones, explaining eruption dynamics and post-eruptive hazards like gas anomalies.
Area of Science:
- * Geophysics
- * Volcanology
- * Remote Sensing
Background:
- * La Palma, Canary Islands, experienced its largest historical volcanic eruption in 2021.
- * Volcanic unrest preceded the eruption, necessitating detailed study.
Purpose of the Study:
- * To analyze the 2021 La Palma volcanic unrest using Interferometric Synthetic Aperture Radar (InSAR).
- * To compare InSAR results with crustal structure for improved interpretation.
- * To explain the eruption's location, characteristics, and associated hazards.
Main Methods:
- * Interferometric Synthetic Aperture Radar (InSAR) data acquisition and analysis for 2021.
- * Development of an improved interpretation methodology for InSAR data.
- * Integration of crustal structure models with InSAR observations.
Main Results:
- * Identified shallow magma accumulation starting 3.5 months before the eruption.
- * Characterized the magma accumulation zone as low-density, fractured rock.
- * Successfully reproduced the final phase of volcanic unrest and detected failed eruption paths.
Conclusions:
- * The study explains the eruption's location and characteristics by linking magma dynamics to crustal structure.
- * Failed eruption paths help explain post-eruptive phenomena, including gas anomalies in La Bombilla and Puerto Naos.
- * Findings enhance understanding of Canarian volcanic activity and volcano monitoring globally, informing hazard assessment and urban planning.
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