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A re-analysis of the
Late Bronze Age eruption and tsunami
of Santorini, Greece, and the
implications for the volcano-tsunami hazard
Dale Dominey-Howes
Journal of Volcanology and Geothermal Research
Volume 130, Issues 1-2,
15 February 2004, Pages 107-132
Abstract: The paroxysmal eruption of Santorini (ca. 3500 BP), referred to as the Late Bronze Age (LBA) eruption, probably generated multiple tsunami; their occurrence and impacts being cited frequently in scientific papers and articles. This paper examines what is known about any LBA tsunami, noting possible mechanisms of generation and identifying sedimentological traces. Firstly, the eruption sequence is outlined providing the context in which tsunami genesis may have occurred. Secondly, the arguments forwarded for the tsunami and a summary of the evidence is given. Thirdly, results of a new geological investigation for LBA tsunami deposits at 41 coastal sites from Crete and Kos are presented. The data are used to test the hypothesis that the LBA eruption generated an east Mediterranean-wide tsunami. It will be seen that no terrestrial geological evidence is identified. The paper re-examines the original arguments presented for LBA tsunami, challenging them because their founding assumptions are flawed. Together, the new data and the re-analysis of the original tsunami hypothesis indicate that there is insufficient evidence to demonstrate that any significant far-field tsunami propagated throughout the entire east Mediterranean as frequently purported. Some terrestrial evidence exists to suggest localised near-field tsunami inundation. There is good submarine evidence however, to suggest that a tsunami was focused to the W and WSW. The results have important implications for understanding the volcano-related tsunami hazard within the region and elsewhere.
Identification of Aniakchak (Alaska) tephra
in Greenland ice core
challenges the 1645 BC date
for Minoan eruption of Santorini
Nicholas J. G. Pearce
John A. Westgate and Shari J. Preece
Warren J. Eastwood
William T. Perkins
Minute shards of volcanic glass recovered from the 1645 Â± 4 BC layer in the Greenland GRIP ice core have recently been claimed to originate from the Minoan eruption of Santorini [Hammer et al., 2003]. This is a significant claim because a precise age for the Minoan eruption provides an important time constraint on the evolution of civilizations in the Eastern Mediterranean. There are however significant differences between the concentrations of SiO2, TiO2, MgO, Ba, Sr, Nb and LREE between the ice core glass and the Minoan eruption, such that they cannot be correlatives. New chemical analyses of tephra from the Late Holocene eruption of the Aniakchak Volcano in Alaska, however, show a remarkable similarity to the ice core glass for all elements, and this eruption is proposed as the most likely source of the glass in the GRIP ice core. This provides a precise date of 1645 BC for the eruption of Aniakchak and is the first firm identification of Alaskan tephra in the Greenland ice cores. The age of the Minoan eruption of Santorini, however, remains unresolved.

“Even when, during the respective Thera Conferences, individual scientists had pointed out that the magnitude and significance of the Thera eruption must be estimated as less than previously thought, the conferences acted to strengthen the original hypothesis. The individual experts believed that the arguments advanced by their colleagues were sound, and that the facts of a natural catastrophe were not in doubt... All three factors reflect a fantasy world rather than cool detachment, which is why it so difficult to refute the theory with rational arguments.” — Eberhard Zangger, “The Future of the Past”, pp 49-50.

(this April topic appears to be the oldest FR thread regarding Sandi MacGillivray; thanks again for sending the Discovery story link, I’m nearly caught up with my back mail)