The transformation of alluvial marshes since 1800 to today In 1800 the Manfredonia plain to the mouth of the Ofanto river was characterised by estensive marshes formed by the water of the torrents which come from the Dauno Sub-Appennines, the Gargano and springs. Due to a lack of slope near to the mouth of the Ofanto, these watercourses caused extensive flooding and in some cases, situations similar to small deltas.
The economic activities that were carried out in these areas were the pasture of buffalo and horses, fishing, hunting and the collection of various natural products such as reeds, wild herbs for food, frogs, snails and other molluscs. The reclamation which began at the end of 1800 and above all from the 1930s onwards carried out by the Capitanata Reclamation Consortium brought about structural changes to all of the Capitanata wetlands.
The Manfredonia wetlands were the last to be reclaimed. Before the regimentation and reclamation works the territory was crossed with the final tracts of the Candelaro, Cervaro and Carapelle torrents which led to the marshes (that is, depressions on the flat areas of the Tableland where more or less perennial springs surface) to then contribute to the formation of coastal lakes such as the Contessa Lake, the Pantano Salso, the Verzentino Lake and the Siponto Pantano which were contiguous and thought to cover an area (including winter flooding) of at least 30.000 hectares.
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