Abstract

Cyprus has a long history of tsunami activity, as described in archaeological and geological records. Although the study area has experienced tsunamis in the past and constitutes an area threatened by this hazard both from the Cyprean arc and from the neighboring Hellenic arc, field research on tsunami evidence on the coastal zone of Cyprus still remains scarce. It is clear from the literature that large boulder accumulations are an important feature along the coasts of Cyprus, testifying to extreme events. A detailed field survey revealed that at various locations cited in the literature as hosting geomorphological evidence of past tsunamis, no such evidence was identified. It is likely that the high touristic activity that has been occurring on the coasts of Cyprus during the last 20 years may have affected tsunami indicators such as boulder accumulations. Tsunamis are unpredictable and infrequent but potentially large-impact natural disasters. The latest strong tsunami that caused damage to the Cypriot coast was centuries ago, when the population and economic growth and development at the Cypriot shoreline did not exist. Today, the coastal zone hosts a higher population as well as increasing touristic activity, highlighting the need for better preparedness, awareness raising and for tsunami-related risk reduction.

Highlights

  • Coasts located at regions with intense tectonic forces are exposed to high vulnerabilities and hazards

  • We aim to provide a better understanding of the tsunami hazard in Cyprus as well as to identify research gaps that should be investigated in the future

  • In general, which takes into consideration the source probability and the tsunami potential, has shown that the total tsunami hazard is significant both from crustal sources, and along coasts near subduction zones, and they may constitute the main origin for various areas in the Mediterranean [46,47,48,62,70,71]

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Summary

Introduction

Coasts located at regions with intense tectonic forces are exposed to high vulnerabilities and hazards. The most frequently noted indicators are boulders, which may be found primarily on the west and southeast coasts of Cyprus In this context, this work aims to provide an overview of palaeo-tsunamis and their field evidence on the coastal zone of Cyprus through an extensive literature review and the discussion of relevant of field data. Two main zones are identified [39]: (i) in south Cyprus, seismic activity takes place along the Cyprean arc, and the generation of tsunamis is favored primarily by seismogenic sources underwater by co-seismic fault dislocations, and (ii) in the Levantine Sea northwards from Gaza, where tsunamirelated earthquakes are primarily related to the left-lateral strike-slip fault system of the Levantine rift; in this case, the seismogenic sources are terrestrial and not submarine, and a mechanism that generates tsunamis has yet to be explained. In general, which takes into consideration the source probability and the tsunami potential, has shown that the total tsunami hazard is significant both from crustal sources, and along coasts near subduction zones, and they may constitute the main origin for various areas in the Mediterranean [46,47,48,62,70,71]

Historic Record of Tsunamis in Cyprus
Warning System and Tsunami Risk for Cyprus Coasts
Findings
Concluding Remarks
Full Text
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