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reasonable to infer that no large earthquakes (Mw
5), in addition to those
of 1117, 1222 and, possibly, 1396, should be missing in the study area after the
1117 event.
In conclusion, the historical data do not significantly help to constrain the as-
sessment of the seismogenic potential of the area, which remains one of the most
unknown, although potentially dangerous, seismic areas of the Italian region.
≥
5
.
Acknowledgments
This paper summarises the investigation performed by a number of investi-
gators, who allowed improving the understanding of the seismicity of the area. We are indebted
with Jean Vogt for sending material form countless European libraries and for encouraging our
work. We are also grateful to P. Galli, who participated to the archaeoseismological surveys in
the Bolzano and Trento provinces, and to the reviewers who helped improving the quality of the
original ms.
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