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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4149

Authors: Behncke, B.*
Neri, M.*
Title: The July-August 2001 eruption of Mt. Etna (Sicily)
Title of journal: Bulletin of Volcanology
Series/Report no.: /65 (2003)
Publisher: Springer-Verlag
Issue Date: 27-Mar-2003
DOI: 10.1007/s00445-003-0274-1
URL: http://www.springerlink.com/content/kq1gw0rpc4v8vht1/?p=07d9868b42cb45ce9842a223cb7b23e7&pi=0
Keywords: Mt. Etna
2001 eruption
Lava flow-field evolution
Central-lateral vs. eccentric activity
Phreatomagmatism
Eruption dynamics
Abstract: The July-August 2001 eruption of Mt. Etna stimulated widespread public and media interest, caused significant damage to tourist facilities, and for several days threatened the town of Nicolosi on the S flank of the volcano. Seven eruptive fissures were active, five on the S flank between 3050 and 2100 m altitude, and two on the NE flank between 3080 and 2600 m elevation. All produced lava flows over various periods during the eruption, the most voluminous of which reached a length of 6.9 km. Mineralogically the 2001 lavas fall into two distinct groups, indicating that magma was supplied through two different and largely independent pathways, one extending laterally from the central conduit system through radial fissures, the other being a vertically ascending eccentric dike. Furthermore one of the eccentric vents, at 2570 m elevation, was the site of vigorous phreatomagmatic activity as the dike cut through a shallow aquifer, both during the intial and closing stages of the eruption. For six days the magma column feeding this vent was more or less effectively sealed from the aquifer, permitting powerful explosive and effusive magmatic activity. While the eruption was characterized by a highly dynamic evolution, complex interactions between some of the eruptive fissures, and changing eruptive styles, its total volume (~25 x 106 m3 of lava and 5-10 x 106 m3 of pyroclastics) was relatively small in comparison with other recent eruptions of Etna. Effusion rates were calculated on a daily basis and reached peaks of 14-16 m3 s-1 while the average effusion rate at all fissures was about 11 m3 s-1, which is not exceptionally high. The eruption showed a number of peculiar features, but none of these (except the contemporaneous lateral and eccentric activity) represented a significant deviation from Etna's eruptive behavior in the long term. However, the 2001 eruption could be but the first in a series of flank eruptions, some of which might be more voluminous and hazardous. Placed in a long-term context, the eruption confirms a distinct trend, initiated during the past 50 years, toward higher production rates and more frequent eruptions, which might bring Etna back to similar levels of activity as during the early to mid 17th century.
Appears in Collections:Papers Published / Papers in press
04.04.09. Structural geology
04.07.99. General or miscellaneous
04.08.99. General or miscellaneous
04.08.01. Gases
04.08.03. Magmas
04.08.05. Volcanic rocks
04.08.06. Volcano monitoring
04.08.08. Volcanic risk
05.02.03. Volcanic eruptions

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