 The unexpected spates of the Lesina caused several floodings in the past decades, resulting in damages to private and public properties; the municipal administration had thereafter renovated the embankments in the early 2000s, thus avoiding further floodings.The actual geomorphology of the area is chiefly due to the perpetual deposit of debris and material by the Brembo River and its tributaries descending from the Prealps located few kilometers to the north.The soil is thus of alluvial origin, mostly made up of gravel and grit in the proximity of Brembo River, clayey in the southerner part of the territory beyond Lesina torrent, rich in humus in the remaining territory.