The analysis of the influence of pumice shape on its terminal velocity

Pumice particles represent the basic “ingredient” of many large explosive eruptions and form as a result of magma fragmentation inside the conduit. At the onset of eruption, fragmental pumices are expelled at high velocity from the crater by the overpressure of gas liberated on explosion. The result...

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Veröffentlicht in:	Geophysical research letters 2005-11, Vol.32 (21), p.L21306.1-n/a
Hauptverfasser:	Dellino, Pierfrancesco, Mele, Daniela, Bonasia, Rosanna, Braia, Giuseppe, La Volpe, Luigi, Sulpizio, Roberto
Format:	Artikel
Sprache:	eng
Schlagworte:	Earth sciences Earth, ocean, space Exact sciences and technology
Online-Zugang:	Volltext
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