Tsunami generation by a rapid entrance of pyroclastic flow into the sea during the 1883 Krakatau eruption, Indonesia

Author:

Maeno Fukashi,Imamura Fumihiko

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference68 articles.

1. Transport of pyroclastic flows across the sea during the explosive, rhyolitic eruption of the Kos Plateou Tuff, Greece;Allen;Bull. Volcanol.,2001

2. ETOPO1 1 Arc-Minute Global Relief Model: Procedures, data sources and analysis;Amante;NOAA Tech. Memo. NESDIS NGDC,2009

3. Volcanic tsunami;Beget,2000

4. The dynamics and thermodynamics of large ash flows;Bursik;Bull. Volcanol.,1996

5. Discussion of a new hypothesis for the Krakatau volcanic eruption in 1883;Camus;J. Volcanol. Geotherm. Res.,1983

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