Abstract
Large boulder accumulations have been observed on various coasts bordering the Mediterranean and have been associated with extreme wave events such as powerful storms or tsunamis. This study provides an in-depth analysis of 430 boulder deposits, located along a 3.5 km stretch of rocky coast situated on the SE of the Maltese Islands. It includes a geomorphometric analysis of the observed boulders and use of numerical modelling to estimate wave height required to initiate boulder movement. Comparisons of aerial imagery over a period of 46 years have made it possible to identify boulder movement that could only be attributed to storm waves, given that no local tsunamigenic event has been recorded over this time period. Positioned in the central Mediterranean, the Maltese Islands are exposed to potential tsunamis generated by seismic activity associated with the Malta Escarpment, and the Calabrian and Hellenic arcs. Although imprints from historic tsunami impact cannot be excluded, results indicate that the area is exposed to strong storm waves that are capable of displacing some of the very large boulders observed on site.
Similar content being viewed by others
References
Agius de Soldanis G (1746) Gozo, ancient and modern, religious and profane. (Mercieca A, Farrugia G, 1999, Trans.). Media Centre, Blata l-Bajda, Malta
Baldassini N, Di Stefano A (2016) Stratigraphic features of the Maltese Archipelago: a synthesis. Nat Hazards. doi:10.1007/s11069-016-2334-9
Barbano MS, Pirrotta C, Gerardi F (2010) Large boulders along the south-eastern Ionian coast of Sicily: storm or tsunami deposits? Mar Geol 275(1–4):140–154
Barbano MS, Gerardi F, Pirrotta C (2011) Differentiation between boulders deposited by tsunamis and storm waves along the south-eastern Ionian coast of Sicily (Italy). Boll Geof Teor Appl 52:707–728
Benner R, Browne T, Brueckner H, Scheffers A, Kelletat D (2010) Boulder transport by waves: progress in physical modelling. Ann Geomorphol 54(3):127–146
Biolchi S, Furlani S et al (2013) Large boulders accumulation along the NE Maltese coast: stormwaves or tsunami event. In: 8th International conference (IAG) on geomorphology, geomorphology and sustainability. Paris, France, 27–31 August 2013, pp 259 (Abstract only)
Biolchi S, Furlani S et al (2016) Boulder accumulations related to extreme wave events on the eastern coast of Malta. Nat Hazards Earth Syst Sci. doi:10.5194/nhessd-3-5977-2015
Blair TC, McPherson JG (1999) Grain size and textural classification of coarse sedimentary particles. J Sediment Res 69(1):6–19
Bryant EA (2001) Tsunami the underrated hazard. Cambridge University Press, Cambridge
Camilleri DH (2006) Tsunami construction risks in the mediterranean—outlining Malta’s scenario. Disaster Prev Manag 15(1):46–162
Causon Deguara J (2015) A study of shore deposits on the coastline between Xgħajra and Żonqor–Marsascala, Unpublished Masters of Arts Dissertation, Department of Geography, University of Malta
Causon Deguara J, Gauci R (2014) Boulder and megaclast deposits on the south-east coast of Malta: signature of storm or tsunami event? In: Benincasa F (ed) Proceedings fifth international symposium monitoring on mediterranean coastal areas: problems and measurement techniques, 17–19 June 2014, Livorno, Italy, CNR-IBIMET, Florence, Italy, pp 594–603
Dalal N, Torab M (2013) Large boulders deposits on the coast of Ras El Hekma, NW Coast, Egypt. Storm or Tsunami? In: The 2nd international symposium on Kaz Mountains and Edremit, May 2–4, 2013, Edremit-Balikesir-Turkey
Drago A (2009) Sea level variability and the ‘Milghuba’ seiche oscillations in the northern coast of Malta, Central Mediterranean. Phys Chem Earth 34:948–970
Drago A, Azzopardi J, Gauci A, Tarasova R, Bruschi A (2013) Assessing the offshore wave energy potential for the Maltese Islands. In: Sustainable Energy 2013: The ISE Annual Conference. 21 March 2013 Qawra, Malta
Engel M, May SM (2012) Bonaire’s boulder fields revisited: evidence for holocene tsunami impact on the Leeward Antilles. Quat Sci Rev 54:126–141
Etienne S, Paris R (2010) Boulder accumulations related to storms on the south coast of the Reykjanes Peninsula (Iceland). Geomorphology 114(1–2):55–70
Furlani S et al (2010) Large boulder along the NE Maltese Coast: tsunami or strom wave deposits? In: Micallef A (ed). J Coast Res, Special Issue No. 61:470 (Abstract only)
Galdies C (2011) The climate of Malta: statistics, trends and analysis 1951–2010. Natl Stat Off, Malta
Galea P (2007) Seismic history of the Maltese Islands and considerations on seismic risk. Ann Geophys 50(6):724–740
Goto K, Okada K, Imamura F (2009) Characteristics and hydrodynamics of boulders transported by storm waves at Kudaka Island. Jpn Mar Geol 262(1–4):14–24
Goto K, Miyagi K, Kawamata H, Imamura F (2010) Discrimination of boulders deposited by tsunamis and storm waves at Ishigaki Island. Jpn Mar Geol 269(1–2):34–45
Hall AM, Hansom JD, Williams DM, Jarvis J (2006) Distribution, geomorphology and lithofacies of cliff-top storm deposits: examples from the high-energy coasts of Scotland and Ireland. Mar Geol 232(3–4):131–155
ISRM (2007) Suggested method for determination of the Schmidt rebound hardness. In: Ulusay R, Hudson JA (ed) The complete ISRM suggested methods for rock characterization, testing and monitoring: 1974–2006, ISRM & ISRM Turkish National Group, Ankara
Katz O, Reches Z, Roegiers JC (2000) Evaluation of mechanical rock properties using a Schmidt Hammer. Int J Rock Mech Min Sci 37:723
Knight J, Burningham H (2011) Boulder dynamics on an Atlantic-facing rock coastline, northwest Ireland. Mar Geol 283:56–65
Knight J, Burningham H, Barrett-Mold C (2009) The geomorphology and controls on development of a boulder-strewn rock platform, NW Ireland. J Coast Res SI 56 (Proceedings of the 10th International Coastal Symposium), pp 1646–1650. Lisbon, Portugal, ISSN 0749–0258
Lorang MS (2011) A wave-competence approach to distinguish between boulder and megaclast deposits due to storm waves versus tsunamis. Mar Geol 283(1–4):90–97
Maouche S, Morhange C, Meghraoui M (2009) Large boulder accumulation on the Algerian coast evidence tsunami events in the western Mediterranean. Mar Geol 262(1–4):96–104
Mastronuzzi G, Pignatelli C (2012) The boulder berm of Punta Saguerra (Taranto, Italy): a morphological imprint of the Rossano Calabro tsunami of April 24, 1836? Earth Planets Space 64:829–842
Mastronuzzi G, Pignatelli C, Sansò P, Selleri G (2007) Boulder accumulations produced by the 20th of February, 1743 tsunami along the coast of southeastern Salento (Apulia region, Italy). Mar Geol 242(1–3):191–205
Mottershead D, Bray M, Soar P, Farres PJ (2014) Extreme wave events in the central Mediterranean: geomorphic evidence of tsunami on the Maltese Islands. Z Geomorphol 58(3):385–411
Nandasena NAK, Paris R, Tanaka N (2011) Reassessment of hydrodynamic equations: minimum flow velocity to initiate boulder transport by high energy events (storms, tsunamis). Mar Geol 281(1–4):70–84
Nandasena NAK, Tanaka N, Sasaki Y, Osada M (2013) Boulder transport by the 2011 great East Japan tsunami: comprehensive field observations and whither model predictions? Mar Geol 346:292–309
Naylor LA, Stephenson WJ (2010) On the role of discontinuities in mediating shore platform erosion. Geomorphology 114(1–2):89–100
Naylor LA, Coombes MA, Viles HA (2012) Reconceptualising the role of organisms in the erosion of rock coasts: a new model. Geomorphology 157–158:17–30
Naylor LA, Kennedy DM, Stephenson WJ (2014) Synthesis and conclusion to the rock coast geomorphology of the world. In: Kennedy DM, Stephenson WJ, Naylor LA (eds) Rock coast geomorphology: a global synthesis. Geological Society, London, Memoirs, 40, pp 283–286
Naylor LA, Stephenson WJ et al (2016) Geomorphological control on boulder transport and coastal erosion before, during and after an extreme extra-tropical cyclone. Earth Surf Process Landf 41:685–700
Noormets R, Crook KAW, Felton EA (2004) Sedimentology of rocky shorelines: 3. hydrodynamics of megaclast emplacement and transport on a shore platform, Oahu,Hawaii. Sediment Geol 172:41–65
Nott J (2003) Waves, coastal boulder deposits and the importance of the pre-transport setting. Earth Planet Sci Lett 210(1–2):269–276
Paris R et al (2009) Tsunamis as geomorphic crises:lessons from the December 26, 2004 tsunami in Lhok Nga, West Banda Aceh (Sumatra, Indonesia). Geomorphology 104(1–2):59–72
Paris R et al (2010) Boulder and fine sediment transport and deposition by the 2004 tsunami in Lhok Nga (western Banda Aceh, Sumatra, Indonesia): a coupled offshore–onshore model. Mar Geol 268(1–4):43–54
Paris R, Naylor LA, Stephenson WJ (2011) Boulders as a signature of storms on rock coasts. Mar Geol 283(1–4):1–11
Pignatelli C, Sansò P, Mastronuzzi G (2009) Evaluation of tsunami flooding using geomorphologic evidence. Mar Geol 260(1–4):6–18
Scheffers A, Scheffers S (2007) Tsunami deposits on the coastline of west Crete (Greece). Earth Planet Sci Lett 259(3):613–624
Scheffers A et al (2008a) Late holocene tsunami traces on the western and southern coastlines of the Peloponnesus (Greece). Earth Planet Sci Lett 269(1–2):271–279
Scheffers SR, Scheffers A, Kelletat D, Bryant EA (2008b) The holocene paleo-tsunami history of West Australia. Earth Planet Sci Lett 270(1–2):137–146
Scheffers A, Scheffers S, Kelletat D, Browne T (2009) Wave-emplaced coarse debris and megaclasts in Ireland and Scotland: boulder transport in a high-energy littoral environment. J Geol 117(5):553–573
Scheffers A et al (2010) Coastal Boulder deposits at Galway Bay and the Aran Islands,Western Ireland. Ann Geomorphol 54(3):247–279
Scicchitano G, Monaco C, Tortorici L (2007) Large boulder deposits by tsunami waves along the Ionian coast of south-eastern Sicily (Italy). Mar Geol 238(1–4):75–91
Scicchitano G, Pignatelli C et al (2012) Terrestrial laser scanner techniques in the assessment of tsunami impact on the Maddalena peninsula (south-eastern Sicily, Italy). Earth Planets Space 64:889–903
Shah-Hosseini M, Morhange C et al (2013) Coastal boulders in Martigues, French Mediterranean: evidence for extreme storm waves during the little ice age. Z Geomorphol 57(4):181–199
Soloviev S, Solovieva ON, Go CN, Kim KS, Shchetnikov NA (2000) Tsunamis in the Mediterranean Sea 2000 B.C.–2000 A.D. Springer, Dordrecht
Spiske M, Halley RB (2014) A coral-rubble ridge as evidence for hurricane overwash, Anegada (British Virgin Islands). Adv Geosci 38:9–20
Stephenson WJ, Naylor LA (2011) Geological controls on boulder production in a rock coast setting: insights from South Wales, UK. Mar Geol 283:12–24
Sunamura T, Horikawa K (1974) Two dimensional beach transformation due to waves. In: American Society of Civilian Engineers, Proceedings 14th coastal engineering conference, pp 920–938
Switzer AD, Burston JM (2010) Competing mechanisms for boulder deposition on the southeast Australian coast. Geomorphology 114(1–2):42–54
The Times of Malta (2015) New Video-Big waves drag more cars on Cirkewwa quay. http://www.timesofmalta.com/articles/view/20150920/local/new-video-big-waves-drag-more-cars-on-cirkewwa-quay.585212. Accessed 22 May 2016
Tinti S, Armigliato A, Pagnoni G, Zaniboni F (2005) Scenarios of giant tsunamis of tectonic origin in the Mediterranean. ISET J Earthq Technol 42(4):171–188
Torab M, Dalal N (2015) Natural hazards mapping of mega waves on the NW coast of Egypt. In: Jasiewicz J, Zwolinski ZB, Mitasova H (eds) Geomorphometry for geosciences. Adam Mickiewicz University, Poznan, pp 213–216
Trenhaile A (2016) Rocky coasts—their role as depositional environments. Earth Sci Rev. doi:10.1016/j.earscirev.2016.05.001
Acknowledgments
The authors would like to thank Dr Saviour Scerri for his contribution in the identification of lithologies, Prof Aldo Drago from the Physical Oceanography Unit of the University of Malta, Blue Ocean Energy Project and Dexawave Malta for providing wave buoy data and Ms Carol Valentino from the Mapping Unit at Malta Environment and Planning Authority (MEPA). Thanks are also due to Prof John A Schembri (University of Malta) for helpful advice and support in his remit as HOD Geography. Finally, the authors would also like to thank two anonymous reviewers whose suggestions have contributed to significantly enhance the quality of this paper. This produce includes data from Mapping Unit (MEPA) and licensed on behalf of them. The MEPA name of the local planning authority (now changed to Planning Authority) has been retained in this paper, in conformity with the copyright agreement previously signed with MEPA.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Causon Deguara, J., Gauci, R. Evidence of extreme wave events from boulder deposits on the south-east coast of Malta (Central Mediterranean). Nat Hazards 86 (Suppl 2), 543–568 (2017). https://doi.org/10.1007/s11069-016-2525-4
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s11069-016-2525-4