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The 2019–2020 volcanic eruption of Late’iki (Metis Shoal), Tonga
Late’iki (previously known as Metis Shoal) is a highly active volcano in the Tofua arc with at least four temporary island-building eruptions and one submarine eruption in the last 55 years. The most recent eruption, commencing in October 2019, resulted in lava effusion and subsequent phreatic explo...
Autores principales: | , , , , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
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Nature Publishing Group UK
2022
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9076857/ https://www.ncbi.nlm.nih.gov/pubmed/35523824 http://dx.doi.org/10.1038/s41598-022-11133-8 |
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author | Yeo, I. A. McIntosh, I. M. Bryan, S. E. Tani, K. Dunbabin, M. Metz, D. Collins, P. C. Stone, K. Manu, M. S. |
author_facet | Yeo, I. A. McIntosh, I. M. Bryan, S. E. Tani, K. Dunbabin, M. Metz, D. Collins, P. C. Stone, K. Manu, M. S. |
author_sort | Yeo, I. A. |
collection | PubMed |
description | Late’iki (previously known as Metis Shoal) is a highly active volcano in the Tofua arc with at least four temporary island-building eruptions and one submarine eruption in the last 55 years. The most recent eruption, commencing in October 2019, resulted in lava effusion and subsequent phreatic explosions, the construction of a short-lived island that was quickly eroded by wave action and possibly further phreatic activity that continued into January 2020. The two-pyroxene dacite from the 2019 eruption is similar to the 1967/8 eruptions suggesting the magma is residual from earlier eruptions and has not undergone further differentiation in the last 50 years. New observations of the 2019 eruption site confirm the lava-dominant character of the volcano summit but a thin veneer of wave-reworked, finely fragmented lava material remains that is interpreted to have been produced by phreatic explosions from hot rock-water interactions during the effusive eruption. A notable absence of quench-fragmented hyaloclastite breccias suggests that non-explosive quench fragmentation processes were minimal at these shallow depths or that hyaloclastite debris has resedimented to greater depths beyond our summit survey area. |
format | Online Article Text |
id | pubmed-9076857 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2022 |
publisher | Nature Publishing Group UK |
record_format | MEDLINE/PubMed |
spelling | pubmed-90768572022-05-08 The 2019–2020 volcanic eruption of Late’iki (Metis Shoal), Tonga Yeo, I. A. McIntosh, I. M. Bryan, S. E. Tani, K. Dunbabin, M. Metz, D. Collins, P. C. Stone, K. Manu, M. S. Sci Rep Article Late’iki (previously known as Metis Shoal) is a highly active volcano in the Tofua arc with at least four temporary island-building eruptions and one submarine eruption in the last 55 years. The most recent eruption, commencing in October 2019, resulted in lava effusion and subsequent phreatic explosions, the construction of a short-lived island that was quickly eroded by wave action and possibly further phreatic activity that continued into January 2020. The two-pyroxene dacite from the 2019 eruption is similar to the 1967/8 eruptions suggesting the magma is residual from earlier eruptions and has not undergone further differentiation in the last 50 years. New observations of the 2019 eruption site confirm the lava-dominant character of the volcano summit but a thin veneer of wave-reworked, finely fragmented lava material remains that is interpreted to have been produced by phreatic explosions from hot rock-water interactions during the effusive eruption. A notable absence of quench-fragmented hyaloclastite breccias suggests that non-explosive quench fragmentation processes were minimal at these shallow depths or that hyaloclastite debris has resedimented to greater depths beyond our summit survey area. Nature Publishing Group UK 2022-05-06 /pmc/articles/PMC9076857/ /pubmed/35523824 http://dx.doi.org/10.1038/s41598-022-11133-8 Text en © The Author(s) 2022 https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) . |
spellingShingle | Article Yeo, I. A. McIntosh, I. M. Bryan, S. E. Tani, K. Dunbabin, M. Metz, D. Collins, P. C. Stone, K. Manu, M. S. The 2019–2020 volcanic eruption of Late’iki (Metis Shoal), Tonga |
title | The 2019–2020 volcanic eruption of Late’iki (Metis Shoal), Tonga |
title_full | The 2019–2020 volcanic eruption of Late’iki (Metis Shoal), Tonga |
title_fullStr | The 2019–2020 volcanic eruption of Late’iki (Metis Shoal), Tonga |
title_full_unstemmed | The 2019–2020 volcanic eruption of Late’iki (Metis Shoal), Tonga |
title_short | The 2019–2020 volcanic eruption of Late’iki (Metis Shoal), Tonga |
title_sort | 2019–2020 volcanic eruption of late’iki (metis shoal), tonga |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9076857/ https://www.ncbi.nlm.nih.gov/pubmed/35523824 http://dx.doi.org/10.1038/s41598-022-11133-8 |
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