The measurement and study campaigns initiated by the Consorzio Venezia Nuova in the second half of the 1980s showed lagoon morphology to be in a worrying state of degradation as a result of the annual loss of a million cubic metres of sediment per year. Since the beginning of the 1900s, half the existing salt marshes have disappeared and a general deepening of the shallows and silting up of the channels has been triggered, in turn triggering and encouraging the diffuse expansion of the tides, to the detriment of natural directional propagation along the network of channels.
A generalised deepening of the lagoon bed (partly caused by the subsidence and eustatism which have increased the mean depth of the lagoon basin by 23 cm in the space of a century) has increased wind-generated wave motion, one of the main mechanisms of erosion. So, diversion of rivers away from the lagoon, a drop in land level and a rise in sea level on one hand, and on the other, dredging of large shipping channels, in particular the Canale Malamocco-Marghera (completed in 1970) have created conditions which encourage transformation of the lagoon into a bay.
Through the acquisition of maps, bathymetric and photogrammetric surveys and studies of lagoon hydrodynamics, the work of the Information Service has enabled the actual situation of the lagoon morphology to be understood and analysis tools able to record transformations of the area to be set up.
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