Article: New science data have been reported by scientists at University of Rome.

"The eruptive style of volcanoes is the result of a complex process, which begins at depth and ends with the arrival of magma with variable amount of volatiles at the Earth's Surface. The amount of gas, the magma composition, and the supply rate are the main factors controlling the either effusive or explosive character of an eruption," scientists writing in the journal Bollettino di Geofisica Teorica Ed Applicata report.

"Degassing during the ascent favors a non-explosive eruptive style. Magma may reside in crustal magma chambers for a long time and may be subject to cooling processes with differentiation and separation of batches having different ...

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