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Etna to the Aeolian Islands (Sicily): importance     Pirazzoli P.A., Mastronuzzi G., Saliege, J.F.,
and evolution of a lithospheric discontinuity.       Sanso P., 1997. Late Holocene emergence in
Acta Vulcanologica 9 (1/2), 113–120.                 Calabria, Italy. Marine Geology 141, 61–70.

Lanzafame, G., Neri, M. and Rust, D. 1996.           Romano R., (1979). Geological Map of Mt. Etna.
Active tectonics affecting the eastern flank of      CNR, Progetto Finalizzato Geodinamica, Istituto
Mount Etna: structural interactions at a regional    Internazionale di Vulcanologia, Catania, 1:50000
and local scale. Pages 25-33 in: Gravestock, P       scale.
and McGuire, W. Etna: fifteen years on;
proceedings of conference Cheltenham and             Rust, D., and Kershaw, S. 2000. Holocene
Gloucester College of Higher Education, UK.          tectonic uplift patterns in northeastern Sicily:
                                                     evidence from marine notches in coastal outcrops
Lentini, F., 1982. The geology of the Mt. Etna       Marine Geology: 167, 105-126.
basement. Memorie della Societa Geologica
Italiana 23, 7–25.                                   Stewart, I.S., Cundy, A., Kershaw, S., & Firth, C.
                                                     (1997) Holocene coastal uplift in the Taormina
Kershaw, S. (2000). Quaternary reefs of              area, northeastern Sicily: implica-tions for the
northeastern Sicily: structure and growth controls   southern prolongation of the Calabrian
in an unstable tectonic setting. Journal of Coastal  seismogenic belt. Journal of Geodynamics: 24,
Research: 16, 1037-1062.                             37–50.

Mauz, B., Buccheri, G., Zoller, L. and Greco, A.,    Valensise, G., Pantosti, D., 1992. A 125 kyr-long
(1997). Middle to upper Pleistocene                  geological record of seismic source repeatability:
morphostructural evolution of the NW-coast of        the Messina Straits (southern Italy) and the
Sicily : thermoluminescence dating and               earthquake (Ms 7.5). Terra Nova 4, 472–483.
paleontological stratigraphical evaluations of
littoral deposits, Palaeogeogr. Palaeoecol.,         Part of the text of this volume came from : Rust
Palaeogeogr., 128, 269-285.                          & Kershaw 2000, Antonioli et al 2002 a, b ,
                                                     Antonioli et al. 2003a, Lanzafame et al. 1996.
Molinier, R., Picard, J., 1953. Notes biologiques a
propos d’un voyage d’etude sur les cotes de          Figure Caption
Sicile. Ann. Inst. Oceanogr. 28, 4, 163–188.
                                                     Fig. 1 Regional geology and tectonic of Sicily.
Monaco, C., Tapponier, P., Tortorici, L., Gillot,
P.Y., (1997). Late Quaternary slip rates on the      Fig 2 The organizers of this field-trip (Kershaw,
Acireale Piedimonte normal faults and tectonic       Rust, Renda and Antonioli). On the background
origin of Mt. Etna (Sicily). Earth and Planetary     Taormina terraces is looked.
Science Letters 147, 125–139.
                                                     Fig. 3 Marine tidal notch at Cala Mancina (St.
Monaco C., Bianca M., Catalano S., De Guidi G.       Vito) 8 m b.s.l.
& Tortorici L. (2002) Sudden change in the Late
Quaternary tectonic regime in eastern Sicily:        Fig. 4 A submerged cave at -30 m on the St. Vito
evidences from geological and geomorphological       Promontory showing a stalagmite with serpulids
features. Boll. Soc. Geol. It., Volume speciale      overgrowth.
n.1, 901-913.
                                                     Fig. 5 Aeolian calcarenites of Lower Pleistocene
Monaco C., Antonioli F., De Guidi G., Lambeck        age containg Elephas and Hippopotamus.
K., Tortorici L. & Verrubbi V. (2003) Sea-level
change and tectonic uplift during the Holocene in    Fig. 6 The inner margin of a submerged terrace
the Catania Plain (eastern Sicily). Congresso "Il    well carved between -15\18 m around all St. Vito
contributo delle antiche linee di riva alla          Promontory.
comprensione della dinamica recente". Abstract
volume, 34.                                                                                                     9
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