The ephemeral fumarolic mineralization of the 2021 Tajogaite volcanic eruption (La Palma, Canary Islands, Spain)

Abstract The present work aims to characterize the ephemeral mineral assemblage related to the fumarolic fields of the Tajogaite volcano, formed in 2021 in La Palma Island (Canary Islands, Spain). A set of 73 samples was obtained after two sampling campaigns in different fumarole sectors of the stud...

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Main Authors: Marc Campeny, Inmaculada Menéndez, Jordi Ibáñez-Insa, Jesús Rivera-Martínez, Jorge Yepes, Soledad Álvarez-Pousa, Jorge Méndez-Ramos, José Mangas
Format: Article
Language:English
Published: Nature Portfolio 2023-04-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-023-33387-6
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author Marc Campeny
Inmaculada Menéndez
Jordi Ibáñez-Insa
Jesús Rivera-Martínez
Jorge Yepes
Soledad Álvarez-Pousa
Jorge Méndez-Ramos
José Mangas
author_facet Marc Campeny
Inmaculada Menéndez
Jordi Ibáñez-Insa
Jesús Rivera-Martínez
Jorge Yepes
Soledad Álvarez-Pousa
Jorge Méndez-Ramos
José Mangas
author_sort Marc Campeny
collection DOAJ
description Abstract The present work aims to characterize the ephemeral mineral assemblage related to the fumarolic fields of the Tajogaite volcano, formed in 2021 in La Palma Island (Canary Islands, Spain). A set of 73 samples was obtained after two sampling campaigns in different fumarole sectors of the studied area. Mineralization related to these fumaroles formed efflorescent patches located at variable distance from the main volcanic craters. Distal patches are predominantly whitish, while in the vicinities they typically show yellowish to orange colours. Field observations also revealed that fumaroles usually occur in elevated topographic areas as well as over fractured and porous volcanic pyroclastic materials. The mineralogical and textural characterisation of the Tajogaite fumaroles unfolds a complex mineral assemblage, comprising cryptocrystalline phases related to low (< 200 °C) and medium temperature (200–400 °C) conditions. In Tajogaite, we propose a classification of three different fumarolic mineralization types: (1) fluorides and chlorides located in proximal fumarolic areas (~ 300–180 °C); (2) native sulphur associated with gypsum, mascagnite and salammoniac (~ 120–100 °C) and (3) sulphates and alkaline carbonates typically occurred in distal fumarolic areas (< 100 °C). Finally, we present a schematic model of the formation of Tajogaite fumarolic mineralization and their compositional evolution developed during the cooling of the volcanic system.
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spelling doaj.art-7edacf739bd5403aa0a9cbc0c4f662082023-04-23T11:18:05ZengNature PortfolioScientific Reports2045-23222023-04-0113111410.1038/s41598-023-33387-6The ephemeral fumarolic mineralization of the 2021 Tajogaite volcanic eruption (La Palma, Canary Islands, Spain)Marc Campeny0Inmaculada Menéndez1Jordi Ibáñez-Insa2Jesús Rivera-Martínez3Jorge Yepes4Soledad Álvarez-Pousa5Jorge Méndez-Ramos6José Mangas7Departament de Mineralogia, Museu de Ciències Naturals de BarcelonaInstituto de Oceanografía y Cambio Global, IOCAG, Dept. de Física, Universidad de Las Palmas de Gran CanariaGeosciences Barcelona (GEO3BCN), Spanish Council for Scientific Research (CSIC)Agencia Estatal de InvestigaciónInstituto de Oceanografía y Cambio Global, IOCAG, Dept. de Física, Universidad de Las Palmas de Gran CanariaGeosciences Barcelona (GEO3BCN), Spanish Council for Scientific Research (CSIC)Instituto de Materiales y Nanotecnología, Departamento de Física, Universidad de La LagunaInstituto de Oceanografía y Cambio Global, IOCAG, Dept. de Física, Universidad de Las Palmas de Gran CanariaAbstract The present work aims to characterize the ephemeral mineral assemblage related to the fumarolic fields of the Tajogaite volcano, formed in 2021 in La Palma Island (Canary Islands, Spain). A set of 73 samples was obtained after two sampling campaigns in different fumarole sectors of the studied area. Mineralization related to these fumaroles formed efflorescent patches located at variable distance from the main volcanic craters. Distal patches are predominantly whitish, while in the vicinities they typically show yellowish to orange colours. Field observations also revealed that fumaroles usually occur in elevated topographic areas as well as over fractured and porous volcanic pyroclastic materials. The mineralogical and textural characterisation of the Tajogaite fumaroles unfolds a complex mineral assemblage, comprising cryptocrystalline phases related to low (< 200 °C) and medium temperature (200–400 °C) conditions. In Tajogaite, we propose a classification of three different fumarolic mineralization types: (1) fluorides and chlorides located in proximal fumarolic areas (~ 300–180 °C); (2) native sulphur associated with gypsum, mascagnite and salammoniac (~ 120–100 °C) and (3) sulphates and alkaline carbonates typically occurred in distal fumarolic areas (< 100 °C). Finally, we present a schematic model of the formation of Tajogaite fumarolic mineralization and their compositional evolution developed during the cooling of the volcanic system.https://doi.org/10.1038/s41598-023-33387-6
spellingShingle Marc Campeny
Inmaculada Menéndez
Jordi Ibáñez-Insa
Jesús Rivera-Martínez
Jorge Yepes
Soledad Álvarez-Pousa
Jorge Méndez-Ramos
José Mangas
The ephemeral fumarolic mineralization of the 2021 Tajogaite volcanic eruption (La Palma, Canary Islands, Spain)
Scientific Reports
title The ephemeral fumarolic mineralization of the 2021 Tajogaite volcanic eruption (La Palma, Canary Islands, Spain)
title_full The ephemeral fumarolic mineralization of the 2021 Tajogaite volcanic eruption (La Palma, Canary Islands, Spain)
title_fullStr The ephemeral fumarolic mineralization of the 2021 Tajogaite volcanic eruption (La Palma, Canary Islands, Spain)
title_full_unstemmed The ephemeral fumarolic mineralization of the 2021 Tajogaite volcanic eruption (La Palma, Canary Islands, Spain)
title_short The ephemeral fumarolic mineralization of the 2021 Tajogaite volcanic eruption (La Palma, Canary Islands, Spain)
title_sort ephemeral fumarolic mineralization of the 2021 tajogaite volcanic eruption la palma canary islands spain
url https://doi.org/10.1038/s41598-023-33387-6
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