Sinkhole Geohazard In Deformed Sulphates at Marina di Lesina (Gargano Promontory, Italy): a Combination of Anthropogenic, Lithologic, and Structural Causes

Sinkhole development and collapse of underground caves within a gypsum substrate is focused in proximity to the beach resort of Marina di Lesina on the Adriatic coast of Southern Italy. This situation constitutes a serious geohazard for the local community and a threat to the development of the tourist activity. Fast sinkhole development has been reported in the last two decades both in terms of newly formed cavities and of widening of already existing ones. It is well known that the presence of structures, such as fault and fractures, focuses fluid flow and intensifies the dissolution and the karst evolution processes. An alignment of the sinkholes as well as their shape anisotropy, west of the harbour canal, suggests also a strong structural control.