Numerical simulation of tsunami generation by pryoclastic flow at Aniakchak Volcano, Alaska

Details Numerical simulation of tsunami generation by pryoclastic flow at Aniakchak Volcano, Alaska Numerical simulation of tsunami generation by pryoclastic flow at Aniakchak Volcano, Alaska

Jul 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003georl..30noce5w&link_type=abstract

Geophysical Research Letters, Volume 30, Issue 14, pp. OCE 5-1, CiteID 1751, DOI 10.1029/2003GL017220

Physics

Geophysics

8

Oceanography: Physical: Tsunamis And Storm Surges, Volcanology: Ash Deposits, Mathematical Geophysics: Modeling

Scientific paper

Pyroclastic flows entering the sea are plausible mechanisms for tsunami generation at volcanic island arcs worldwide. We evaluate tsunami generation by pyroclastic flow using an example from Aniakchak volcano in Alaska where evidence for tsunami inundation coincident with a major, caldera-forming eruption of the volcano ca. 3.5 ka has been described. Using a numerical model, we simulate the tsunami and compare the results to field estimates of tsunami run up.

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