ITaly HAzards from CApable faulting
Italy is one of most active regions of the Mediterranean area in
terms of active tectonics and seismicity. Several historical
catastrophic earthquakes (e.g., 1693 Eastern Sicily, 1783 Calabria,
1805 Bojano, 1908 Messina and 1915 Fucino events) reached MCS
intensities of XI (magnitude ca. or slightly above 7).
Paleoseismological studies have been able to find and characterize
the causative faults of several of these events, and have
demonstrated that latest Pleistocene-Holocene displacements have
affected many structures considered silent before.
The estimation of hazard derived from earthquakes and surface
faulting is an important issue especially in densely populated and
industrialized areas as the Italian territory is.
Consequently, mapping and characterizing capable faults assume a
key role for the risk mitigation. To this purpose, the Geological
Survey of Italy - APAT (Italian Agency for Environment Protection
and for Technical Services) has developed the ITHACA project (ITaly
HAzard from CApable faults).
ITHACA is a database aimed at collecting and analyzing all
available information on active tectonic structures in Italy, with
particular regard to tectonic processes able to generate natural
hazards. The project deals with active capable faults, which are
defined as faults that have significant potential for displacement
at or near the ground surface.
The database of capable faults is an important tool for a)
environmental and seismic hazards analysis, b) understanding of
evolving landscape, c) land-use planning, d) Civil Protection
emergency management. Moreover, it provides further elements for a
more precise evaluation of geodynamic processes.
The first release of ITHACA database was presented during the
2000 IGC in Rio. Since then, the work has continued to improve the
database. Presently, there is not a new comprehensive version
available. However, many data on Northern and Southern Italy have
changed. Many faults have been reviewed, some removed, others
added. More information is available on many faults. More
specifically, so far this review has regarded Northern Italy,
where, although historically seismicity has been less relevant with
respect to peninsular Italy, the density of population and
infrastructures and the results of new specialist studies suggest a
level of risk far from negligible and hence demand more attention
even in areas considered quiet before. A significant improvement
has received the database for Calabria and Sicily. For the latter
also some offshore structures have been introduced (so far, Ionian
Sea and Sicily Channel), which, despite the modest knowledge, are
certainly active and capable of producing significant effects,
including tsunamis, in the surrounding coastal areas.
Work is ongoing to update data also in the rest of Italy.
ITHACA database