Between 2015 and 2019, a team of archaeologists, palaeobotanists and geologists from the Universities of Groningen, Amsterdam and Leiden looked into the distal effects of a powerful eruption of the Somma–Vesuvius volcano in Campania on the former wetlands of the Agro Pontino and Fondi coastal plains in Central Tyrrhenian Italy. These wetlands are located c. 60 km south of Rome and between 90 and 140 km north-west of Mount Vesuvius. The ‘Avellino’ eruption took place during an advanced stage of the Early Bronze Age and was radiocarbon dated around 1900 BCE. This article reports on the results of the research programme “The Avellino Event: Cultural and Demographic Effects of the Great Bronze Age Eruption of Mount Vesuvius”, funded by the Dutch Research Council. The team’s main hypothesis, that people living in the surroundings of Mount Vesuvius in the Early Bronze Age who had time to escape the proximal effects of the eruption – pyroclastic flows and heavy ash falls – fled to the relative safety of nearby coastal areas to build a temporary or permanent new existence, was disproved by field evidence early on. No major environmental and archaeological impacts were evident in the archaeological and environmental record of the study area around the date of the eruption. Nonetheless, the research resulted in a significant increase in geological and palaeobotanical data, which has proved extremely useful for the reconstruction of the longue durée of human–landscape interactions. The Avellino tephra was a most reliable chronological horizon in this reconstruction contributing to the overall objectives of the long-running Pontine Region Project of the University of Groningen. This contribution contains an overview of the main results of the Avellino Event Project, including an overview of scientific publications, valorisation output, and a brief discussion of some remarkable spin-off projects.
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