Considering the characteristics of the Strombolian behaviour and the classical
intermittency, we suggest that the well-known superposition of tremor and explosion-quakes of
the volcanic activity can be described as an intermittent phenomenon. Indeed, a slightly modified
non-linear map of Venkataramani et al. (Phys. Rev. Lett., 77 (1996) 5361), characterized by
an intermittent behaviour, reproduces the statistical features of the experimental time series
associated with the Strombolian activity, matching the distributions of the amplitude (size) and
of the inter-times between two successive explosions
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