Discrete magma injections drive the 2021 La Palma eruption

Author:

Ubide Teresa1ORCID,Márquez Álvaro2ORCID,Ancochea Eumenio2ORCID,Huertas María José2ORCID,Herrera Raquel3ORCID,Coello-Bravo Juan Jesús4ORCID,Sanz-Mangas David25ORCID,Mulder Jack16ORCID,MacDonald Alice1ORCID,Galindo Inés5ORCID

Affiliation:

1. The University of Queensland, School of the Environment; Brisbane, Australia.

2. Universidad Complutense, Área de Petrología y Geoquímica; Madrid, Spain.

3. Universidad Rey Juan Carlos, ESCET, Área de Geología, Tecvolrisk Research Group; Móstoles, Madrid, Spain.

4. Fundación Telesforo Bravo - Juan Coello; Puerto de la Cruz, Tenerife, Spain.

5. Instituto Geológico y Minero de España (IGME-CSIC); Las Palmas de Gran Canaria, Spain.

6. University of Adelaide, School of Physical Sciences; Adelaide, Australia.

Abstract

Understanding the drivers of the onset, evolution, and end of eruptions and their impact on eruption style is critical in eruption forecasting and emergency management. The composition of erupted liquids is a key piece of the volcano puzzle, but untangling subtle melt variations remains an analytical challenge. Here, we apply rapid, high-resolution matrix geochemical analysis on samples of known eruption date spanning the entire 2021 La Palma eruption. Sr isotope signatures reveal distinct pulses of basanite melt driving the onset, restart, and evolution of the eruption. Elemental variations in matrix and microcrysts track progressive invasion, and draining, of a subcrustal crystal mush. Associated variations in lava flow rate, vent development, seismicity, and SO 2 emission demonstrate that volcanic matrix resolves eruption patterns that could be expected in future basaltic eruptions globally.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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