Site effect is usually associated with local geologi- cal conditions, which increase or decrease the level of shaking compared with standard attenuation relations. We made an attempt to see in the macroseismic data of Italy some other effects, namely, hot/cold spots in the terminology of OLSEN (in Bull. Seismol. Soc. Am. 90, 6B, 577–594, 2000), which are related to local fault geometry rather than to soil conditions. We give a list of towns and villages liable to amplify (?) or to reduce (–) the level of shaking in comparison with the nearby settlements. Relief and soil condi- tions cannot always account for the anomalous sites. Further, there are sites where both (?) and (–) effects are observed depending on the earthquake. The opposite effects can be generated by events from the same seismotectonic zone and along the same direction to the site. Anomalous sites may group themselves into clusters of different scales. All isolated anomalous patterns presented in this paper can be used in hazard analysis, in particular, for the modeling and testing of seismic effects.
