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Keywords: Santorini, Thera, Minoan eruption, radiocarbon dating, tree-rings Debate J.H., K.P. FOSTER, G. STEINHAUSER & M. org//science.
Aitken, H. Michael, P. Betancourt, and P. Gauss, M. Lindblom, R. Smith, and J. Wright eds. Balmuth and R. Tykot eds.
Post-eruptive flooding of Santorini caldera and implications for tsunami generation
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The Minoan eruption was a major catastrophic volcanic eruption that devastated the Aegean island of Thera (now called Santorini) in Despite the evidence, the exact date of the eruption has been difficult to determine. Bruce Bowen: Mycenae and Minoan Crete, ,; ^ Jump up to: Foster, KP, Ritner, RK, and Foster, BR.
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Lesson 17: Bibliography
Santorini is a dominant expression of magma generation and subsequent volcanism in the Meditereanean area, where a calk-alkaline, high-alumina, basalt-andesite-dacite type of volcanism was expressed from eight centres. The volcanics of the Akrotiri peninsula are considered to be the products of the earliest Pliocene Pleistocene volcanic centre.
The present study has investigated the mineral chemistry of some major pyrogenic phenocrysts, such as plagioclase and Fe-Ti oxides, of the Akrotiri pyroclatics unit, which have undergone a notable zeolitization procedure. The results are compatible with magma mixing mechanism of a primitive mantle derived, saturated, of mafic composition component with silicic magma in shallow crustal depths.
Foster, K. P. ‘Volcanic echoes in ancient Near Eastern texts’, in Cultural responses to the volcanic landscape: the Mediterranean and beyond, M. S.
Absolute Chronology of the Late Bronze Age in the Aegean
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Caldera-forming eruptions of island volcanoes generate tsunamis by the interaction of different eruptive phenomena with the sea. Such tsunamis are a major hazard, but forward models of their impacts are limited by poor understanding of source mechanisms. The caldera-forming eruption of Santorini in the Late Bronze Age is known to have been tsunamigenic, and caldera collapse has been proposed as a mechanism.
Here, we present bathymetric and seismic evidence showing that the caldera was not open to the sea during the main phase of the eruption, but was flooded once the eruption had finished. Inflow of water and associated landsliding cut a deep, 2. If, as at most such volcanoes, caldera collapse occurred syn-eruptively, then it cannot have generated tsunamis. Entry of pyroclastic flows into the sea, combined with slumping of submarine pyroclastic accumulations, were the main mechanisms of tsunami production.
Repeated effusive eruptions since the LBA eruption have built up the Kameni Volcano within the resulting caldera 6. Other subdivisions of these same layers have been published Orange box outlines the area of the northwest strait, shown as b a slope gradient map, c a tangential curvature map and d a flowline density map.
Post-eruptive flooding of Santorini caldera and implications for tsunami generation
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Such tsunamis are a major hazard, but forward models of their impacts are limited by poor understanding of source mechanisms. The caldera-forming eruption of Santorini in the Late Bronze Age is known to have been tsunamigenic, and caldera collapse has been proposed as a mechanism. Here, we present bathymetric and seismic evidence showing that the caldera was not open to the sea during the main phase of the eruption, but was flooded once the eruption had finished.
Inflow of water and associated landsliding cut a deep, 2.
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The total amount of literature about Santorini would probably fill an own library. I recommend a visit to Fira’s municipal library on Thera itself just opposite the bus station! This list is necessarily incomplete, but includes the most important works. Contributions are highly welcome. Please contact me Tom Pfeiffer!
As key references I suggest the reader to start with one of the following:.
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The Minoan eruption was a major catastrophic volcanic eruption that devastated the Aegean island of Thera now called Santorini in around BCE. Although there are no clear ancient records of the eruption, the Minoan eruption may have been alluded to in the Egyptian Tempest Stele ,  as well as the Chinese Bamboo Annals. Geological evidence shows the Thera volcano erupted numerous times over several hundred thousand years before the Minoan eruption. In a repeating process, the volcano would violently erupt, then eventually collapse into a roughly circular seawater-filled caldera , with numerous small islands forming the circle.
The caldera would slowly refill with magma, building a new volcano, which erupted and then collapsed in an ongoing cyclical process. Immediately before the Minoan eruption, the walls of the caldera formed a nearly continuous ring of islands, with the only entrance between Thera and the tiny island of Aspronisi. The northern part of the caldera was refilled by the volcanic ash and lava, then collapsed again.
The volcano ejected up to four times as much as the well-recorded eruption by Krakatoa in The Thera volcanic events and subsequent ashfall probably destroyed all indigenous life, as occurred on Krakatoa. This layer has three distinct bands that indicate the different phases of the eruption. The thinness of the first ash layer, along with the lack of noticeable erosion of that layer by winter rains before the next layer was deposited, indicate that the volcano gave the local population a few months’ warning.
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Betancourt, V. Karageorghis, R. Laffineur, and W. Niemeier eds. Betancourt, M. Nelson, and H. Williams eds. Bietak and E.