2010
DOI: 10.1016/j.margeo.2010.05.005
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Large boulders along the south-eastern Ionian coast of Sicily: Storm or tsunami deposits?

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Cited by 134 publications
(147 citation statements)
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“…Along the coast of Vendicari, 40 km south of Siracusa ( Fig. 1(a)), Barbano et al (2010) discovered a boulder field and isolated boulders related to different tsunami events. Moreover, tsunami impact deposits related to the 1693 event and other tsunami and storm deposits were found preserved within a ria-type rocky coastal setting at the bottom of the channel harbour of Ognina, 20 km south of Siracusa (Scicchitano et al, 2010).…”
Section: Geological and Geomorphological Settingmentioning
confidence: 99%
See 1 more Smart Citation
“…Along the coast of Vendicari, 40 km south of Siracusa ( Fig. 1(a)), Barbano et al (2010) discovered a boulder field and isolated boulders related to different tsunami events. Moreover, tsunami impact deposits related to the 1693 event and other tsunami and storm deposits were found preserved within a ria-type rocky coastal setting at the bottom of the channel harbour of Ognina, 20 km south of Siracusa (Scicchitano et al, 2010).…”
Section: Geological and Geomorphological Settingmentioning
confidence: 99%
“…In the boulder accumulation process, is the impacting wave height more important compared to the wave length and to the wave period? Different theories have been proposed in the recent time, but the final reply is still far away (Nott, 2003;Goto et al, 2007Goto et al, , 2009bGoto et al, , 2010bHansom et al, 2008;Imamura et al, 2008;Pignatelli et al, 2009;Barbano et al, 2010). The more easy reply is that if a wave can be described by height, length and period, the best way to evaluate its impact on a rocky coast should consider these parameters all together.…”
Section: Introductionmentioning
confidence: 99%
“…Is the impacting wave height more important of the wave length and of the wave period in the possibility to shape boulders accumulation? Different theories have been proposed in the recent time but the final reply is still far away (Goto et al, 2007;2009;Hansom et al, 2008;Pignatelli et al, 2009;Barbano et al, 2010). The more immediate reply is that if a wave can be described by height, length and period the best way to evaluate its impact on a rocky coast should consider these parameters all together.…”
Section: Discussionmentioning
confidence: 99%
“…Recent hydrodynamic theories tried to put in relation boulders and coastal features to the wave responsible for their accumulation developing mathematical formulas. Starting from the boulders size and shape, knowing the local waveclimate, it should be possible to discriminate between storm and tsunami inland scattering (Nott, 1997(Nott, , 2003Noormets et al, 2002Noormets et al, , 2004Pignatelli et al, 2009;2010a,b;Imamura et al, 2008;Barbano et al, 2010).…”
Section: Morphological Effect Of Past Tsunamimentioning
confidence: 99%
“…While there is no ambiguity for observations of recent tsunamis (Goff et al, 2006;Goto et al, 2007), large boulder accumulations may be associated with historic and prehistoric events related to tsunamis (Nott, 2000;Mastronuzzi and Sansò, 2000;Williams and Hall, 2004;Mastronuzzi et al, 2007;Maouche et al, 2009;Paris et al, 2009). Nevertheless, we cannot rule out the possibility of transport by storms (Barabano et al, 2010), and some recent case studies show the role of storm waves in forming boulder accumulations worldwide (Noormets et al, 2002;Nott, 2004;Goto et al, 2009Goto et al, , 2011Suanez et al, 2009;Etienne and Paris, 2010).…”
Section: Introductionmentioning
confidence: 88%