Abstract
Vulsini Volcano, Bolsena District, central Italy is a Quaternary centre eruptions of which have been dominated by the production of ignimbrites. Stratigraphic studies show that there are six major ignimbrite units with individual minimum volumes of 0.5 to 3 km3 and a large number of smaller ignimbrite units, together with pyroclastic surge and pyroclastic fall deposits. It is estimated that at least 90% of the volcanic products are pyroclastic producing a low profile volcano with 1 to 5‡ slopes.
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