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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.
Afiliação
  • Yeo IA; National Oceanography Centre Southampton, Southampton, UK. i.yeo@noc.ac.uk.
  • McIntosh IM; Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Tokyo, Japan.
  • Bryan SE; School of Earth and Atmospheric Sciences, Queensland University of Technology, Brisbane, Australia.
  • Tani K; National Museum of Nature and Science (Kahaku), Tokyo, Japan.
  • Dunbabin M; School of Electrical Engineering and Robotics, Queensland University of Technology, Brisbane, Australia.
  • Metz D; Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Tokyo, Japan.
  • Collins PC; Queens University Belfast, Belfast, UK.
  • Stone K; Vava'u Environmental Protection Association (VEPA), Vava'u, Tonga.
  • Manu MS; Natural Resources Division, Tonga Ministry of Lands, Survey and Natural Resources, Nuku'alofa, Tonga.
Sci Rep ; 12(1): 7468, 2022 05 06.
Article em En | MEDLINE | ID: mdl-35523824
ABSTRACT
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.
Assuntos

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Assunto principal: Erupções Vulcânicas / Desastres Idioma: En Revista: Sci Rep Ano de publicação: 2022 Tipo de documento: Article País de afiliação: Reino Unido

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Assunto principal: Erupções Vulcânicas / Desastres Idioma: En Revista: Sci Rep Ano de publicação: 2022 Tipo de documento: Article País de afiliação: Reino Unido