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The results of a comparison of the spirit levelling data made by I.G.M. in 1967 and in 1970, are presented. An analysis of these data shows that the altitude variations of bench marks in the considered triennial period seem to originate from the collective rotation of an inclined plane, which intersects the geoid surface with an azimuth of 43° to the North. This is in accordance with the orientation of the fault pattern given by local geology. The fact that the existing bench marks were sited along the coastline, and the lack of a comparison with data relative to motion on more compact geological structures, lead necessarily to provisional conclusions

Vertical movements along the northwestern side of Messina straits, in the 1967-1970 period