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   <subfield code="a">Stratigraphic constraints for explosive activity in the past 100ka at Etna Volcano, Italy</subfield>
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   <subfield code="c">[Mauro Coltelli, Paola Del Carlo, Luigina Vezzoli]</subfield>
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   <subfield code="a">Abstract.: The pyroclastic deposits of Etna have been correlated over the whole volcanic edifice for the first time, allowing the construction of a continuous record of tephra-producing events, which extends from approximately 100ka to the Present. In this interval, five main periods of explosive activity have been identified: (a) ∼100-ka strombolian to subplinian activity; (b) 80- to 100-ka plinian benmoreitic activity; (c) 16- to 80-ka strombolian to subplinian from basaltic to mugearitic activity; (d) 15.5- to 15-ka plinian benmoreitic activity accompanying the caldera-forming eruptions of the Ellittico Volcano; and (e) the most recent 13-ka basaltic explosive activity of strombolian and subplinian type of the present edifice that also includes the 122-B.C. plinian eruption. This study results in a semi-quantitative and in some cases quantitative definition of the intensity and chronology of the explosive activity at Etna. Moreover, this work gives a new significance to the volcanic hazards of Etna, a volcano generally considered to be the site of gentle effusive eruptions.</subfield>
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   <subfield code="a">Tephrostratigraphy Tephrochronology Basaltic explosive eruptions Tephra marker beds Y1 tephra layer X4 tephra layer Quaternary Etna</subfield>
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   <subfield code="a">Coltelli</subfield>
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   <subfield code="u">CNR, Istituto Internazionale di Vulcanologia, piazza Roma 2, 95123 Catania, Italy</subfield>
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   <subfield code="a">Del Carlo</subfield>
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