Post-eruptive flooding of Santorini caldera and implications for tsunami generation

The Bronze Age eruption of Santorini is known to have generated tsunamis with caldera collapse as the likely mechanism. However, new bathymetric and seismic data presented by Nomikou et al. show that the entry of pyroclastic flows into the sea is the most likely tsunami-generating mechanism at Santo...

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Autores principales: P. Nomikou, T. H. Druitt, C. Hübscher, T. A. Mather, M. Paulatto, L. M. Kalnins, K. Kelfoun, D. Papanikolaou, K. Bejelou, D. Lampridou, D. M. Pyle, S. Carey, A. B. Watts, B. Weiß, M. M. Parks
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Lenguaje:EN
Publicado: Nature Portfolio 2016
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Acceso en línea:https://doaj.org/article/dbdd5ecc6acb43daa423c0dded90b04a
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spelling oai:doaj.org-article:dbdd5ecc6acb43daa423c0dded90b04a2021-12-02T15:35:00ZPost-eruptive flooding of Santorini caldera and implications for tsunami generation10.1038/ncomms133322041-1723https://doaj.org/article/dbdd5ecc6acb43daa423c0dded90b04a2016-11-01T00:00:00Zhttps://doi.org/10.1038/ncomms13332https://doaj.org/toc/2041-1723The Bronze Age eruption of Santorini is known to have generated tsunamis with caldera collapse as the likely mechanism. However, new bathymetric and seismic data presented by Nomikou et al. show that the entry of pyroclastic flows into the sea is the most likely tsunami-generating mechanism at Santorini.P. NomikouT. H. DruittC. HübscherT. A. MatherM. PaulattoL. M. KalninsK. KelfounD. PapanikolaouK. BejelouD. LampridouD. M. PyleS. CareyA. B. WattsB. WeißM. M. ParksNature PortfolioarticleScienceQENNature Communications, Vol 7, Iss 1, Pp 1-10 (2016)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
P. Nomikou
T. H. Druitt
C. Hübscher
T. A. Mather
M. Paulatto
L. M. Kalnins
K. Kelfoun
D. Papanikolaou
K. Bejelou
D. Lampridou
D. M. Pyle
S. Carey
A. B. Watts
B. Weiß
M. M. Parks
Post-eruptive flooding of Santorini caldera and implications for tsunami generation
description The Bronze Age eruption of Santorini is known to have generated tsunamis with caldera collapse as the likely mechanism. However, new bathymetric and seismic data presented by Nomikou et al. show that the entry of pyroclastic flows into the sea is the most likely tsunami-generating mechanism at Santorini.
format article
author P. Nomikou
T. H. Druitt
C. Hübscher
T. A. Mather
M. Paulatto
L. M. Kalnins
K. Kelfoun
D. Papanikolaou
K. Bejelou
D. Lampridou
D. M. Pyle
S. Carey
A. B. Watts
B. Weiß
M. M. Parks
author_facet P. Nomikou
T. H. Druitt
C. Hübscher
T. A. Mather
M. Paulatto
L. M. Kalnins
K. Kelfoun
D. Papanikolaou
K. Bejelou
D. Lampridou
D. M. Pyle
S. Carey
A. B. Watts
B. Weiß
M. M. Parks
author_sort P. Nomikou
title Post-eruptive flooding of Santorini caldera and implications for tsunami generation
title_short Post-eruptive flooding of Santorini caldera and implications for tsunami generation
title_full Post-eruptive flooding of Santorini caldera and implications for tsunami generation
title_fullStr Post-eruptive flooding of Santorini caldera and implications for tsunami generation
title_full_unstemmed Post-eruptive flooding of Santorini caldera and implications for tsunami generation
title_sort post-eruptive flooding of santorini caldera and implications for tsunami generation
publisher Nature Portfolio
publishDate 2016
url https://doaj.org/article/dbdd5ecc6acb43daa423c0dded90b04a
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