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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10073

Authors: Sulpizio, R.*
Groppelli, G.*
Insinga, D.*
Branca, S.*
Del Carlo, P.*
Tamburrino, S.*
Zanchetta, G.*
Title: The Large Explosive Activity of Mt. Etna as Recorded in Distal Tephrostratigraphy
Editors: Rocha, R.; Faculdade de Ciências e Tecnologia Ciências da Terra, Universidade Nova de Lisboa
Pais, J.; Faculdade Ciências e Tecnologia Ciencias da Terra, Universidade Nova de Lisboa
Kullberg, J. C.; Ciências da Terra, Faculdade de Ciências e Tecnologia
Finney, S.; Geological Sciences, California State University Long Beach
Issue Date: 2014
Publisher: Springer International Publishing
URL: http://link.springer.com/chapter/10.1007%2F978-3-319-04364-7_245
DOI: 10.1007/978-3-319-04364-7_245
Keywords: Mount Etna
Tephrostratigraphy
Explosive eruptions
Mediterranean area
Abstract: Mt. Etna is renowned for being the most active and highest volcano in Europe. Lava flows and weak explosive eruptions characterize its activity, but intermediate to large explosive eruptions have punctuated its eruptive history. Marine and lacustrine distal records are excellent archives for the recognition of past large explosive activity at Mt. Etna, as testified by the recognition of distal tephra layers of Pleistocene to Holocene age. These data are, to date, neither organised nor correlated to the proximal stratigraphic and chronological records. Here, we propose the reorganisation and correlation of the distal tephra layers from Mt. Etna in order to decipher the timings and frequency of its major explosive eruptions.
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