Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6597
AuthorsD’Oriano, C.* 
Bertagnini, A.* 
Pompilio, M.* 
TitleAsh erupted during normal activity at Stromboli (Aeolian Islands, Italy) raises questions on how the feeding system works
Issue Date2010
DOI10.1007/s00445-010-0425-0
URIhttp://hdl.handle.net/2122/6597
KeywordsStromboli
Strombolian activity
Ash
Paroxysms
Clast morphology
Glass chemistry
Bubble ascent
Subject Classification04. Solid Earth::04.04. Geology::04.04.05. Mineralogy and petrology 
04. Solid Earth::04.08. Volcanology::04.08.08. Volcanic risk 
AbstractAsh fallout collected during 4 days of sampling at Stromboli confirms that a crystal-rich (HP) degassed magma erupts during the Strombolian explosions that are characteristic of the normal activity of this volcano. We identified 3 different types of juvenile ash fragments (fluidal, spongy and dense), which formed through different mechanisms of fragmentation of the low-viscosity, physically heterogeneous (in terms of the size and spatial distribution of bubbles) shoshonitic magma. A small amount (less than 3 vol%) of volatile-rich magma with low porphyricity (LP), erupted as highly vesicular ash fragments, has been collected, together with the HP magma, during normal strombolian explosions. Laboratory experiments and the morphological, textural and compositional investigations of ash fragments reveal that the LP ash is fresh and not recycled from the last paroxysm (15 March 2007). We suggest that small droplets of LP magma are dragged to the surface by the time-variable but persistent supply of deep derived CO2-rich gas bubbles. This coupled ascent of bubbles and LP melts is transient and does not perturb the dynamics of the HP magma within the shallow reservoir. This finding provides a new perspective on how the Stromboli volcano works and has important implications for monitoring strategies.
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