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Explosive eruption, flank collapse and megatsunami at Tenerife ca. 170 ka
Giant mass failures of oceanic shield volcanoes that generate tsunamis potentially represent a high-magnitude but low-frequency hazard, and it is actually difficult to infer the mechanisms and dynamics controlling them. Here we document tsunami deposits at high elevation (up to 132 m) on the north-w...
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| Gepubliceerd in: | Nat Commun |
|---|---|
| Hoofdauteurs: | , , , , |
| Formaat: | Artigo |
| Taal: | Inglês |
| Gepubliceerd in: |
Nature Publishing Group
2017
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| Onderwerpen: | |
| Online toegang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5440666/ https://ncbi.nlm.nih.gov/pubmed/28504256 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms15246 |
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