Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/2964
Authors: Di Vito, M. A.* 
Sulpizio, R.* 
Zanchetta, G.* 
D’Orazio, M.* 
Title: The late Pleistocene pyroclastic deposits of the Campanian Plain: new insights into the The late Pleistocene pyroclastic deposits of the Campanian Plain: new insights into the explosive activity of Neapolitan volcanoes
Issue Date: 2007
DOI: 10.1016/j.jvolgeores.2007.11.019
URI: http://hdl.handle.net/2122/2964
Keywords: Neapolitan volcanoes
late Pleistocene
explosive eruptions
Somma-Vesuvius
Campi Flegrei,
Ischia island
Subject Classification04. Solid Earth::04.04. Geology::04.04.05. Mineralogy and petrology 
04. Solid Earth::04.04. Geology::04.04.10. Stratigraphy 
04. Solid Earth::04.08. Volcanology::04.08.05. Volcanic rocks 
Abstract: The lithological and compositional characteristics of eighteen different pyroclastic deposits of Campanian origin, dated between 125 cal ka BP and 22 cal ka BP, were described. The pyroclastic deposits were correlated among different outcrops mainly located on the Apennine slopes that border the southern Campanian plain. They were grouped in two main stratigraphic and chronologic intervals of regional significance: a) between Pomici di Base (22.03 cal ka BP; Somma-Vesuvius) and Campanian Ignimbrite (39 cal ka BP; Campi Flegrei) eruptions; and b) older than Campanian Ignimbrite eruption. Three new 14C AMS datings support the proposed correlations. Six eruptions were attributed to the Pomici di Base-Campanian Ignimbrite stratigraphic interval, while twelve eruptions are older than Campanian Ignimbrite. Of the studied deposits two originated from Ischia island, five are related to Campi Flegrei, and three to Somma-Vesuvius. Two eruptions have an uncertain correlation with Somma-Vesuvius or Campi Flegrei, while six eruptions remain of uncertain source. Minimum volumes of five eruptions were assessed, ranging between 0.5 km3 and 4 km3. Two of the studied deposits were correlated with Y-3 and X-5 tephra layers, which are widely dispersed in the central Mediterranean area. The new stratigraphic and chronologic data provide an upgraded chrono-stratigraphy for the explosive activity of Neapolitan volcanoes in the period between 125-22 cal ka BP.
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