On 9 September 1998, at 13: 28 local time (11: 28 UTC), a moderate earthquake ofM w= 5.6
struck the Southern Apennines at the northwest margin of the Pollino Massif (the highest …

The Pollino Range is the southernmost segment of the Southern Apennines at the boundary
with the Calabrian Arc. While several strong earthquakes (magnitude 6.5–7.0) have …

Seismically induced environmental effects (in particular, surface faults, ground cracks, slope
failures, liquefaction, soil compaction, hydrological changes, tsunamis) are assumed to …

The September–October 1997 seismic sequence in the Umbria–Marche regions of Central
Italy (main shocks on September 26, Mw 5.7 and 6.0, and on October 14, Mw 5.6) left …

At 0: 33 and 9: 40 GMT on September 26, 1997 two earthquakes ofM w= 5.5 and M w= 6,
respectively, struck a large area of the central Apennines, between the Umbria and Marche …

The eastern Molise earthquake had an epicentral intensity of Io= 7–8 MCS (Mercalli-
Cancani-Sieberg scale) and a maximum intensity of Imax= 8–9 in the village of San Giuliano …

Moderate to strong crustal earthquakes are generally accompanied by a distinctivepattern of
coseismic geological phenomena, ranging from surface faulting to groundcracks, landslides …

This paper documents evidence of surface faulting associated with the 6 April 2009
moderate-sized earthquake (ML 5.8, M w 6.3) in the central Apennines of Italy, which caused …

A sequence of thousands of small to moderate earthquakes has been occurring since spring
2010 in the Pollino Mountains area, southern Italy (Fig. 1), where a seismic gap was …

Abstract In May 2012, two moderate (-to-strong) earthquakes that were associated with a
noticeable aftershock sequence affected the eastern sector of the Po Plain, Italy, in …