Umbria-Marche region (Central Italy) has been interested by a seismic seque
nce, which caused a large amount of damage within an extensive area (around
5000 km(2)). The sequence produced eight shocks with magnitude higher than
5.0, the largest of them occurring on September 26, UTC 09:40, Ml = 5.8. T
he incidence of many shocks with a magnitude higher than 4.0 contributed to
the creation of a damage pattern that was in evolution for more than one m
onth. Such seismic behavior motivated field operators to perform a real-tim
e macroseismic survey to update the data set. One of the major objectives w
as to differentiate the effects pertaining to each of the largest shocks. I
n this paper we present the macroseismic survey performed during the sequen
ce, along with some preliminary results inferred. Intensity points of seven
of the main shocks are shown, together with the filtered macroseismic fiel
ds produced following the application of specific statistical methods. Fina
lly, consideration is given to the comparison of these study results with c
orresponding tectonic and geological data. (C) 1999 Elsevier Science Ltd. A
ll rights reserved.