Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9064
AuthorsD'Oriano, C.* 
Bertagnini, A.* 
Cioni, R.* 
Pompilio, M.* 
TitleIdentifying recycled ash in basaltic eruptions
Issue Date28-Jul-2014
Series/Report no./4 (2014)
DOI10.1038/srep05851
URIhttp://hdl.handle.net/2122/9064
KeywordsVolcanic Ash
Basaltic eruptions
intra-crater recycling
Subject Classification04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring 
AbstractDeposits of mid-intensity basaltic explosive eruptions are characterized by the coexistence of different types of juvenile clasts, which show a large variability of external properties and texture, reflecting alternatively the effects of primary processes related to magma storage or ascent, or of syn-eruptive modifications occurred during or immediately after their ejection. If fragments fall back within the crater area before being re-ejected during the ensuing activity, they are subject to thermally- and chemically-induced alterations. These ‘recycled’ clasts can be considered as cognate lithic for the eruption/explosion they derive. Their exact identification has consequences for a correct interpretation of eruption dynamics, with important implications for hazard assessment. On ash erupted during selected basaltic eruptions (at Stromboli, Etna, Vesuvius, Gaua-Vanuatu), we have identified a set of characteristics that can be associated with the occurrence of intra-crater recycling processes, based also on the comparison with results of reheating experiments performed on primary juvenile material, at variable temperature and under different redox conditions.
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