Tsunamis boulders on the rocky shores of Minorca (Balearic Islands)

Abstract. Large boulders have been found on marine cliffs of 24 study areas on Minorca, in the Balearic archipelago. These large imbricated boulders of up to 229 t are located on platforms that comprise the rocky coastline of Minorca, several tens of meters from the edge of the cliff, up to 15 m above the sea level and kilometers away from any inland escarpment. They are mostly located on the south-eastern coast of the island, and numerical models have identified this coastline as a zone with a high probability of tsunami impact. The age of the boulders of the studied localities range between 1574 AD and recent times, although most of them are concentrated around the year 1790 AD. Although some storm waves might play a role in their dislodging, the distribution of the boulder sites along the Balearic Islands, the degree and direction of imbrication and the run-up necessary for their placement suggest transport from northern African tsunami waves that hit the coastline of Minorca.

[1]  P. Cox,et al.  Extraordinary boulder transport by storm waves (west of Ireland, winter 2013–2014), and criteria for analysing coastal boulder deposits , 2018 .

[2]  A. Perea,et al.  Morfometría y dinámica de bloques asociados a tsunami en una rampa litoral del Norte de Menorca (Illes Balears) , 2017 .

[3]  R. Gauci,et al.  Evidence of extreme wave events from boulder deposits on the south-east coast of Malta (Central Mediterranean) , 2017, Natural Hazards.

[4]  F. Xavier,et al.  Blocs de tempesta i tsunami a les costes rocoses de les Illes Balears: anàlisi geomorfològica i morfomètrica , 2016 .

[5]  Olaia Iglesias Cerdeira Generación y propagación de tsunamis en el mar Catalano-Balear , 2015 .

[6]  S. Devoto,et al.  Boulder accumulations related to extreme wave events on the eastern coast of Malta , 2015 .

[7]  Mourad Bezzeghoud,et al.  Seismicity of Algeria from 1365 to 2013: Maximum Observed Intensity Map (MOI2014) , 2015 .

[8]  P. Farres,et al.  Extreme wave events in the central Mediterranean: Geomorphic evidence of tsunami on the Maltese Islands , 2014 .

[9]  A. Scheffers,et al.  Stable imbrication and delicate/unstable settings in coastal boulder deposits: Indicators for tsunami dislocation? , 2014 .

[10]  J. L. Casamor,et al.  Tsunami Resonance in Palma Bay and Harbor, Majorca Island, as Induced by the 2003 Western Mediterranean Earthquake , 2014, The Journal of Geology.

[11]  M. Bezzeghoud,et al.  Seismicity along the Azores-Gibraltar region and global plate kinematics , 2014, Journal of Seismology.

[12]  E. Anthony,et al.  Coastal boulders in Martigues, French Mediterranean: evidence for extreme storm waves during the Little Ice Age , 2013 .

[13]  P. Drap,et al.  Large boulders accumulation along the NE Maltese coast: stormwaves or tsunami event? , 2013 .

[14]  S. M. May,et al.  Bonaire's boulder fields revisited: evidence for Holocene tsunami impact on the Leeward Antilles , 2012 .

[15]  C. Pignatelli,et al.  The boulder berm of Punta Saguerra (Taranto, Italy): a morphological imprint of the Rossano Calabro tsunami of April 24, 1836? , 2012, Earth, Planets and Space.

[16]  Giuseppe Mastronuzzi,et al.  Terrestrial Laser Scanner techniques in the assessment of tsunami impact on the Maddalena peninsula (south-eastern Sicily, Italy) , 2012, Earth, Planets and Space.

[17]  J. L. Casamor,et al.  The BIG’95 Submarine Landslide–Generated Tsunami: A Numerical Simulation , 2012, The Journal of Geology.

[18]  S. Devoto,et al.  Large Boulder Along the NE Maltese Coast: Tsunami or Storm Wave Deposits? , 2011 .

[19]  E. Lekkas,et al.  Critical Factors for Run-up and Impact of the Tohoku Earthquake Tsunami , 2011 .

[20]  A. Hall Storm wave currents, boulder movement and shore platform development: A case study from East Lothian, Scotland , 2011 .

[21]  J. A. Álvarez-Gómez,et al.  Tsunami hazard at the Western Mediterranean Spanish coast from seismic sources , 2011 .

[22]  M. S. Barbano,et al.  Large boulders along the south-eastern Ionian coast of Sicily: Storm or tsunami deposits? , 2010 .

[23]  B. Moragues Long-term extreme wave height events in the Balearic Sea: characterization, variability and prediction , 2010 .

[24]  R. Paris,et al.  Boulder accumulations related to storms on the south coast of the Reykjanes Peninsula (Iceland) , 2010 .

[25]  Christophe Morhange,et al.  Large boulder accumulation on the Algerian coast evidence tsunami events in the western Mediterranean , 2009 .

[26]  Giuseppe Mastronuzzi,et al.  Evaluation of tsunami flooding using geomorphologic evidence , 2009 .

[27]  A. Hall,et al.  Magnitude and frequency of extra-tropical North Atlantic cyclones: A chronology from cliff-top storm deposits , 2009 .

[28]  D. Kelletat Comments to Dawson, A.G. and Stewart, I. (2007), Tsunami deposits in the geological record. — Sedimentary Geology 200, 166 183 , 2008 .

[29]  H. Hébert,et al.  The 1856 Djijelli (Algeria) earthquake and tsunami: source parameters and implications for tsunami hazard in the Balearic Islands , 2008 .

[30]  Simon Matthias May,et al.  Late Holocene tsunami traces on the western and southern coastlines of the Peloponnesus (Greece) , 2008 .

[31]  Luigi Cavaleri,et al.  Analysis of the Voyager storm , 2008 .

[32]  Giuseppe Mastronuzzi,et al.  Boulder accumulations produced by the 20th of February, 1743 tsunami along the coast of southeastern Salento (Apulia region, Italy) , 2007 .

[33]  A. Scheffers,et al.  Tsunami deposits on the coastline of west Crete (Greece) , 2007 .

[34]  Giovanni Scicchitano,et al.  Large boulder deposits by tsunami waves along the Ionian coast of south-eastern Sicily (Italy) , 2007 .

[35]  Said Maouche,et al.  The tsunami induced by the 2003 Zemmouri earthquake (MW = 6.9, Algeria): modelling and results , 2006 .

[36]  Lluís Gómez Pujol Patrons, taxes i formes d'erosió a les costes rocoses carbonatades de Mallorca , 2006 .

[37]  A. Jansà,et al.  Towards a climatology of sensitivities of Mediterranean high impact weather − first approach , 2006 .

[38]  A. Jansà,et al.  Intense storms in the Mediterranean: a first description from the ERA-40 perspective , 2006 .

[39]  A. Sanna,et al.  Mediterranean wave climate variability and its links with NAO and Indian Monsoon , 2005 .

[40]  F. Valero,et al.  A high-resolution 44-year atmospheric hindcast for the Mediterranean Basin: contribution to the regional improvement of global reanalysis , 2005 .

[41]  E. Boschi,et al.  An atlas of Mediterranean seismicity , 2004 .

[42]  D. Kelletat,et al.  Sedimentologic and geomorphologic tsunami imprints worldwide—a review , 2003 .

[43]  J. Nott Waves, coastal boulder deposits and the importance of the pre-transport setting , 2003 .

[44]  C. Synolakis,et al.  Tsunami: The Underrated Hazard , 2001 .

[45]  J. M. M. Solares,et al.  Los efectos en España del terremoto de Lisboa (1 de noviembre de 1755) , 2001 .

[46]  B. Levin,et al.  Tsunamis in the Mediterranean Sea 2000 B.C.-2000 A.D. , 2000 .

[47]  S. L. Soloviev Tsunamigenic zones in the Mediterranean Sea , 1990 .

[48]  N. Ambraseys The El Asnam (Algeria) earthquake of 10 October 1980; conclusions drawn from a field study , 1981, Quarterly Journal of Engineering Geology.

[49]  K. Emery Marine Solution Basins , 1946, The Journal of Geology.