Abstract
The presence of self potentials on the upper part of Stromboli Volcano is associated with the existence of convection cells of gases and condensed liquids whose rising parts are situated above the hot zones. A model of a convection cell fed by a hot fluids through its lower middle part was calculated and applied to the various structures of the upper part of the volcano. This model which takes account of a process which is probably fairly common in volcanic system, gives a clear explanation of the various potential zones.
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