The Avellino plinian eruption of Somma-Vesuvius (3760 y.B.P.): the progressive evolution from magmatic to hydromagmatic style
- 1 November 1993
- journal article
- Published by Elsevier in Journal of Volcanology and Geothermal Research
- Vol. 58 (1-4) , 67-88
- https://doi.org/10.1016/0377-0273(93)90102-w
Abstract
No abstract availableThis publication has 9 references indexed in Scilit:
- The Taupo pumice: Product of the most powerful known (ultraplinian) eruption?Published by Elsevier ,2003
- Quantitative models of the fallout and dispersal of tephra from volcanic eruption columnsBulletin of Volcanology, 1986
- Characteristics of dune-bedded pyroclastic surge bedsetsJournal of Volcanology and Geothermal Research, 1984
- A model for Plinian eruptions of VesuviusNature, 1981
- Characteristics of widespread pyroclastic deposits formed by the interaction of silicic magma and waterBulletin of Volcanology, 1978
- Explosive volcanic eruptions — a new classification schemeInternational Journal of Earth Sciences, 1973
- Two Plinian Pumice-Fall Deposits from Somma-Vesuvius, ItalyGSA Bulletin, 1973
- Grain-Size Characteristics of Pyroclastic DepositsThe Journal of Geology, 1971
- The Geology of Monte Somma and Vesuvius, being a Study in VulcanologyQuarterly Journal of the Geological Society, 1884