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Ta b l e 2 Summary of the information available about the 1396 earthquake from historical
compilations
Source
Effects
When
Where
Agnelli, 1895
Strong earthquake; many
buildings collapsed
The day of St.
Stephen, 1397
Lombardia
Tovazzi, 1803
An earthquake happened
26 December 1397
Trento
Tatti, 1683
Strong earthquake; many
buildings collapsed
26 December, the
day of St.
Stephen, 1397
Lombardia
Calvi, 1676
Strong earthquake; many
buildings collapsed
26 December 1397
Bergamo and
Lombardia
Ghilini, 1666
Strong earthquake; many
buildings collapsed
26 December, the
day of St.
Stephen, 1397
Alessandria and
Lombardia
Schiavina, 1616
Strong earthquake; many
buildings collapsed
The day of St.
Stephen (1397)
Alessandria and
Lombardia
Nicolio, 1582
Strong earthquake; many
buildings collapsed
The day of St.
Stephen (1397)
Rovigo and
Lombardia
Corio, 1503
Strong earthquake; many
buildings collapsed
The day of St.
Stephen 1397 (the
year is expressed
according to the
Nativity calendar
style,
corresponding to
1396)
Lombardia
Zagata, 15th cent
Strong earthquakes
26 December 1397
Verona
Mezzotti chronicle
Some houses collapsed
26 November 1396
Monza
ones (Annali della Fabbrica del Duomo di Milano, 1387-1411) and coeval chron-
icles, such as Annales Mediolanenses, 1230-1402; Castelli, 1387-1407, without
success. Only the chronicle (1337-1517) of the Mezzotti family of Monza, pub-
lished in 1840 (Mezzotti, 1840), quoted by Mercalli (1883) with reference to the
presumed “26 November, 1369” event, reports:
“ai 26 di novembre del 1396 si sentı grave scossa di terremoto e rovinarono alcune case”
[on the 26 November 1396 a strong shock was felt and some houses were damaged]
Stucchi and Albini (1988) did not rely on this date and proposed to accept the date of
26 December 1396 according to Corio (1503). Later, Stucchi et al. (1993) assessed
I 7-8 MCS at Monza (Fig. 9). Boschi et al. (1997 and 2000) assigned I 7-8 MCS
at Monza on the basis of the Mezzotti chronicle. Guidoboni and Comastri (2005)
reappraised the analysis and, though confirming the above mentioned intensity at
Monza, concluded that the lack of information from coeval sources in Lombardia
and Veneto suggests that the epicentral location should be considered with caution.
 
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