The Po di Adria River, Frattesina and the Po Delta Between the Middle-Recent Bronze Age and the Early Iron Age
The Southern Verona Lowlands /High-Polesine territories, in the second part of the Sub-Boreal period were subject together with a large part of the Po Plain to continental climatic conditions, interrupted by damp oscillations (Löbben oscillation), finally marked by sub-arid terminal peaks. At the sa...
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| Format: | Article |
| Language: | Italian |
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University of Bologna
2018-12-01
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| Series: | IpoTESI di Preistoria |
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| Online Access: | https://ipotesidipreistoria.unibo.it/article/view/9402 |