Inherent characteristic of the landslide phenomenon, the danger of the landslide is determined by the magnitude (intensity of the phenomenon calculated on the basis of a matrix calculation combined between the velocity and the geometric severity/material involved in the failure) and the probability of occurrence.The danger is divided into 4 classes (P1, P2, P3, P4) as required by current legislation. Where the Plans are binding for the Hydrogeological structure, each class of danger corresponds to a different urban constraint. Please refer to the nomativa PAI for more information.
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