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This is due to the variability of tsunami impacts and the dynamics of post-tsunami processes.
Case studies of recent tsunami impacts have proven to be extremely useful in understanding the geologic processes involved during inundation and return flow, and refining the criteria used to identify paleotsunami deposits in the geologic record.
Among these environments, tsunami impacts in the marine realm are the least known, although, as discussed by Dawson and Stewart (2007), in theory, offshore tsunami deposits may comprise a large percentage of tsunami records in geological history.
Tsunami impacts (erosion) on the seafloor have primarily been examined indirectly through studies of onshore deposits containing marine microfossils such as foraminifera (e.g., Hawkes et al., 2007; Uchida et al., 2010) or diatoms (e.g., Dawson, 2007; Sawai et al., 2009).
Semi structured interviews with local witnesses of the event, field measurements of local features, as well as secondary data sources provided information on wave height at the shoreline, landscape characteristics as well as tsunami impacts inland, i.e. structural damage and maximum flood distance.
We also have info on the Hawaii tsunami evacuation, as well as a live Chile Earthquake page and a larger Tsunami Impacts page.
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Some regional warnings in Hawaii, including one in 1994, have passed with no tsunami impact at all.
Fig. 4. 3D representation of the tsunami impact on a rocky coast.
They begin by focusing on the expected tsunami impact on the coasts of Southern Italy.
Further issues concern the potential of preservation and recognition of offshore tsunami impact.
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