The 1693 earthquake was a disastrous event affecting eastern Sicily, s
outhern Italy, where it caused over 60,000 victims and total destructi
on of several villages and towns in the districts of Siracusa, Ragusa,
and Catania. The earthquake was followed by a tsunami that struck the
Ionian coasts of Sicily and the Messina Strait and was probably obser
ved even in the Aeolian Islands. Historical documents on sea waves and
flooding, though not abundant, allow us to form a picture of the tsun
ami first attack and inundation. The first water movement all along th
e Sicilian coastline was a strong sea withdrawal, followed by a violen
t sea return and coastal flooding. The main purpose of this research i
s to put constraints on the focal mechanism of this earthquake on the
basis of the available documents on the tsunami (1) by simulating tsun
ami from different possible sources via numerical modeling based on fi
nite element technique and shallow water approximation and (2) by choo
sing the source best fitting the tsunami data as the most plausible ca
use for this tsunami. The relevance of this study should also be evalu
ated in light of the circumstance that no certain indication on the ea
rthquake fault can be deduced from the available macroseismic data alo
ne. Solving the source problem for this event, one of the largest occu
rring in southeastern Sicily in historical times, is a significant con
tribution to understanding the seismotectonic regime of the region and
to assessing the related earthquake and tsunami hazard/risk with impl
ications on mitigation policies.