Stratigraphic constraints for explosive activity in the past 100 ka at Etna Volcano, Italy
Stratigraphic constraints for explosive activity in the past 100 ka at Etna Volcano, Italy
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DOI:
10.1007/s005310000117
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发表时间:
2000-12-01
影响因子:
2.3
通讯作者:
Vezzoli, L
中科院分区:
文献类型:
--
作者:
Coltelli, M;Del Carlo, P;Vezzoli, L
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 100 ka to the Present. In this interval, five main periods of explosive activity have been identified: (a) similar to 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 Ij-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.