Geomorphological Processes and Landscape Evolution of the Lagoon of Venice

The Lagoon of Venice, extending along the northern Adriatic coast in northeastern Italy, is the most important Italian lagoon. The delta systems of the Po, Adige and Brenta rivers delineate the lagoon from the south, whilst the Sile and Piave rivers border the lagoon in the north. The lagoon is closed by the barrier islands of Lido and Pellestrina and the spit of Cavallino. Inside the lagoon, several landforms typical of this peculiar environment are present: islands, salt marshes, tidal flats, fluvial deltas, tidal channels, sand dunes, ancient coastlines and man-made forms such as landfills, fish farms, coastal defences and artificial channels. Due to protracted human interference with natural processes, the Lagoon of Venice may be considered today as an artificial environment.