Storm or tsunamis: Boulder deposits on the rocky coasts of the Balearic Islands (Spain)

• Published in: Marine geology Vol. 463; p. 107112
• Main Authors: Roig-Munar, Francesc Xavier, Gelabert, Bernadí, Rodríguez-Perea, Antoni, Martín-Prieto, José Ángel, Vilaplana, Joan Manuel
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01-09-2023
• Subjects: Balearic Islands; Cliff-top boulders; Rocky coasts; Storms; Tsunamis; Rocky coasts; Balearic Islands; Storms; Cliff-top boulders; Tsunamis
• ISSN: 0025-3227; 1872-6151
• DOI: 10.1016/j.margeo.2023.107112

The origin of large imbricate boulders at the edge of coastal cliffs, by storm or tsunamis, is usually controversial. The Balearic Islands are a perfect place to elucidate this origin because the surrounding marine basins have low storm energy compared to oceans, and they are located 250 km N of the main tsunamigenic area of the Western Mediterranean. Thus, there have been recent and historical tsunamis affecting the Balearic Islands, especially in its southern and eastern parts. Tsunami simulations from submarine earthquakes on the North African coast predict the impact of tsunami waves on the Balearic Islands. Large coastal boulders of the Balearic Islands are located in the exact places numerical models predict they will be. Despite the fact that the height and energy of storm waves are much larger from the north and west, these boulders are located in the eastern and southern parts of the islands. Documentary sources confirm a very large tsunami affecting the southeast coast of Majorca in 1756, with a run-in up to 2 km and a run-up up to 45 m. Hydrodynamic equations applied to these boulders results in storm wave height values never recorded in 60 years. In February 2020, the highest storm wave ever recorded (14.33 m) was detected at Minorca buoy, related to storm Gloria. As predicted by hydrodynamic equations, none of the boulders studied moved significantly, and only three new boulders, located at sea level or at the cliff edge, were quarried. According to radiocarbon data and rate of growth of dissolution pans, the year of emplacement of boulders in the studied localities ranges between 1591 CE and 1894 CE. Thus, the distribution of the boulder sites along the islands, the historical record of a large tsunami, the run-up necessary for their placement, and the insignificant boulder movement produced by the highest storm recorded indicates that the cliff-top boulders of the Balearic Islands were quarried by North African tsunami waves.
•Large boulders at the E and S rocky coasts of the Balearic Islands at considerable heights (up to 15 m).•Larger storm energy for the N and W rocky coasts of the Balearic Islands.•Historical tsunami in 1756 described by Fontsere (1919) SE Mallorca with a run-up up to 45 m.•The Balearic Islands are the emerged land closer to tsunamigenic area in the wester Mediterranean.•Gloria storm (2020), the largest storm ever recorded in the E Balearic Islands, not enough for boulder movement.