Eruption dynamics and tephra dispersal from the 24 November 2006 paroxysm at South-East Crater, Mt Etna, Italy

• Published in: Journal of volcanology and geothermal research Vol. 274; pp. 78 - 91
• Main Authors: Andronico, Daniele, Scollo, Simona, Lo Castro, Maria Deborah, Cristaldi, Antonio, Lodato, Luigi, Taddeucci, Jacopo
• Format: Journal Article
• Language: English
• Published: Oxford Elsevier B.V 15.03.2014; Elsevier
• Subjects: 24 November 2006 paroxysm; Ash componentry; Craters; Crystalline rocks; Decoupling; Deposits; Dynamics; Earth sciences; Earth, ocean, space; Exact sciences and technology; Explosions; Fallout; Igneous and metamorphic rocks petrology, volcanic processes, magmas; Lava; Magma/gas decoupling; Mt Etna; Plumes; Tephra deposit; Southern Europe; Italy; Sicily Italy; Mount Etna; Europe; 24 November 2006 paroxysm; Ash componentry; Tephra deposit; Mt Etna; Magma/gas decoupling; volcanic ash; plumes; fine-grained materials; eruption dynamics; strombolian-type eruptions; magmas; tephra; vents; grain size; lava; fallout; craters; style; particles; size distribution
• ISSN: 0377-0273; 1872-6097
• DOI: 10.1016/j.jvolgeores.2014.01.009

Between 30 August and 15 December 2006, Mt Etna, Italy, underwent both effusive and explosive activity which took place from the South-East Crater, one of its summit craters. Several paroxysmal episodes followed in succession, separated by a few days of minor activity and characterised by dissimilar explosive style and intensity. Here, we report one of the most studied and powerful episodes, which started early in the morning on 24 November 2006 and lasted about 13h. Excellent weather conditions enabled reconstructing in detail the onset and evolution of the eruptive phenomena both by live-camera recordings and direct observations. The explosive activity consisted of powerful Strombolian activity alternating with short periods of lava fountains. A weak volcanic plume rose up to ~2km above the volcanic vent, followed by tephra fallout which covered the SE and S flanks of Etna. Campaigns allowed collecting about 40 tephra samples and mapping the fallout deposit. The clockwise shifting of the volcanic plume during the eruption caused the different timing of the fallout on the ground, thus widening the dispersal area. Voronoi's method was used to evaluate: i) the total grain-size distribution, indicating that the fallout deposit peaked at 1 ϕ, and, for the first time at Etna, ii) the total componentry distribution, finding that most of the particles were lithics, with a low proportion of juvenile vs. lithics (34:65). The total erupted mass was estimated ~1.9×108kg, corresponding to a mass eruption rate of ~5×103kgs−1. Physical parameters and textural features of the erupted products suggest that the 24 November 2006 explosive event may be classified as small-sized in the recent history of Etna, and that the eruptive dynamic was mainly governed by magma/gas decoupling, which produced relatively fine-grained fallout deposits containing unusual elongated sideromelane ash particles. •The variation of the volcanic plume during the 24 November 2006 Etna paroxysm•The fine-grained, lithic- and tachylite-enriched ash fallout deposit is described.•The total componentry of the fallout deposit is proposed.•Information on total mass and mass eruption rate of the tephra fallout deposit•Style and classification of explosive activity