On the fate of pumice rafts formed during the 2012 Havre submarine eruption

Pumice rafts are floating mobile accumulations of low-density pumice clasts generated by silicic volcanic eruptions. Pumice in rafts can drift for years, become waterlogged and sink, or become stranded on shorelines. Here we show that the pumice raft formed by the impressive, deep submarine eruption...

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Detalles Bibliográficos
Autores principales: Jutzeler, Martin, Marsh, Robert, Carey, Rebecca J., White, James D. L., Talling, Peter J., Karlstrom, Leif
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2014
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3997806/
https://www.ncbi.nlm.nih.gov/pubmed/24755668
http://dx.doi.org/10.1038/ncomms4660

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3997806/
https://www.ncbi.nlm.nih.gov/pubmed/24755668
http://dx.doi.org/10.1038/ncomms4660

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