Venice lagoon formed part of a network of inland waterways used for navigation in the northern Adriatic, an almost continuous system of lakes, river-mouths and canals, at least partly pre-Roman in origin. The fossae which cross the present lagoon are the continuation of a complex system of natural watercourses and artificial canals between Ravenna and Aquileia. Two Roman buildings discovered on the present San Felice canal could be interpreted as providing navigational assistance at points linking the sea and inland routes.

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Throughout history the Balearic Islands have had different degrees of social connectivity between the islands themselves and between them and the mainland. While the influence of historical dynamics is well documented, less so is the impact of winds, currents, and meteo-marine conditions. This paper analyses the meteo-marine conditions for coastal navigation to better understand how these configured the main maritime routes across the islands. We focus on the seafaring communities of the Balearic Islands in the Bronze Age when a series of sites along the coastline suggest the creation of a network of coastal infrastructure to support maritime mobility.

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