Volcanic Tsunami Hazards: What can the Santorini seafloor tell us?
3,600 years after the great Minoan eruption of Santorini, researchers from GEOMAR Helmholtz Centre for Ocean Research Kiel in an international collaboration, study the marks that have been imprinted in the seafloor around the Greek archipelago to find out what caused an ancient tsunami. Their findings have now been published in the scientific journal Earth and Planetary Science Letters and will contribute to a better tsunami hazard assessment also at other marine volcanoes.
Seismic measurements with Research Vessel R/V Poseidon during cruise POS538 offshore Santorini in October 2019 (photo: Paraskevi Nomikou)
The Minoan eruption of Santorini in the Aegean Sea was one of the largest explosive volcanic eruptions in the Holocene. In the Late Bronze Age, during a disastrous natural catastrophe Santorini tore apart and sent large amounts of hot volcanic rock and gas across the eastern Mediterranean. A massive tsunami devastated the coast of Crete and destroyed many Minoan settlements. Today’s remnants are the island of Santorini with only its large caldera rims sticking out of the sea.
Researchers from GEOMAR Helmholtz Centre for Ocean Research Kiel and colleagues from the University of Rhode Island, the University of Hamburg, the Ocean Discovery League, Saunderstown and the University of Athens studied the marks of this giant cascade of events on the ocean floor to find out what caused the huge tsunami 3,600 years ago.
In October 2019 a team led by marine geophysicist Dr. Jens Karstens collected new geophysical data with research vessel R/V Poseidon from around the Santorini Caldera. With sound waves, they created a structural image of the subsurface. The researchers combined the new seismic profiles with swath bathymetry data collected during several previous international expeditions. These provide information on the water depth and the detailed morphology of the sea floor.
Shaded bathymetric map of the study area. The white lines indicate the location of high-resolution seismic reflection profiles used for this study, that were accomplished during R/V Poseidon cruise in October 2019. Profiles A, B and C can be seen in the figure to the right.
Clearly striking in the high-resolution seismic profiles are wavy sediment structures, so called undulating seafloor bedforms that can be found radially around the caldera and extend up to 25 kilometres from the volcano. In their study, now published in the scientific journal Earth and Planetary Science Letters, the researchers show that these structures are very important to interpret the genesis of volcanic tsunamis.
Volcanic tsunamis have so far been poorly understood due to the complicated cascade of events that is involved in triggering them. “Reconstructing the seafloor morphology is one step forward to a better understanding of the generation of tsunamis during large eruptions”, explains Jens Karstens.
Seafloor bedforms are similar to ripples or dunes that one can observe in river beds or at the beach. They develop at the interface of water and the ocean floor because of sediment being transported by flowing water. In the case at Santorini, the sediments were formed when currents of dense hot gas and volcanic rocks, so called pyroclastic flows, entered the ocean after they flowed at high speeds down the volcanic flanks. Another process that can produce such undulating bedforms is the destabilization of sediments on the volcanic flanks.
“With the analysis of our new seismic reflection data, we were now able to show that actually the deposits around Santorini are not uniform. They are thicker to the north and thinner at the other flanks“, Karstens describes. In the north of Santorini, the undulating seafloor bedforms were formed by pyroclastic flows and on the other flanks the researchers see evidence that these sediment structures are related to instabilities of the volcanic flanks, thought to be formed or reactivated during the Minoan Eruption. “We cannot reconstruct the exact dynamics of the mass movement, in particular, how fast the rock masses slid down the Santorini slopes. However our findings indicate that they contributed to the generation of the destructive Minoan tsunami”, says the geophysicist.
Triggered by a tremor during the large caldera forming eruption, segments of the volcanic slope slid hundreds of metres down the flank. This caused large water masses to be displaced, generating a huge tsunami wave. The researchers estimate the amount of material that moved down the volcanic flanks during the Minoan eruption to have been two cubic kilometres. In comparison, only one tenth of the equivalent total volume was displaced during a recent collapse-generated tsunami at Anak Kraktau in 2018, which devastated the surrounding coasts of the Sunda Strait in Indonesia.
Deformations of the subsurface extending 200 metre deep below the seafloor show that slope instabilities can also be reactivated by regional tectonic earthquakes which have occurred with Magnitudes more than 7 (M7+) in the Santorini area in the past, causing destructive tsunamis.
“This study emphasises the importance of the understanding of flank instabilities for the tsunami hazard assessment at active volcanoes” says professor for marine geomechanics at GEOMAR, Dr. Morelia Urlaub, leader of the project PRE COLLAPSE and co-author of the publication. The Minoan eruption is one of the best-studied volcanic eruptions worldwide and Santorini offers the unique opportunity to relate the formation of the undulating seafloor deposits with the volcanic processes.
In August 2023, members of the PRE COLLAPSE research group will visit Anak Krakatau with the research vessel RV Sonne to make similar seismic and bathymetric surveys to study the 1883 and 2018 eruptions. They will be able to use the newly gained knowledge about the undulating seafloor bedforms to better interpret and compare the subsurface structures at Krakatau and Santorini and evaluate how their findings can be applied for hazard assessment also at other active marine volcanoes.
Original publication:
Formation of undulating seafloor bedforms during the Minoan eruption and their implications for eruption dynamics and slope stability at Santorini
Jens Karstens, Jonas Preine, Steven Carey, Katherine L.C. Bell, Paraskevi Nomikou, Christian Hübscher, Danai Lampridou, Morelia Urlaub
Earth and Planetary Science Letters
Santorini Caldera rim (photo: Jonas Preine)
3D views on seismic profiles combined with morphological grids of the slopes of Santorini. The high-resolution bathymetry was measured from an autonomous underwater vehicle (AUV)
(A) Northern slope of Santorini viewed from the east. The rim of the northern caldera breach is visible on the left side. (B) Northwestern flank of Santorini viewed from the northwest. (C) Southwestern flank of Santorini viewed from the south.
“Reconstructing the seafloor morphology is one step forward to a better understanding of the generation of tsunamis during large eruptions” Jens Karstens
The crew of R/V Poseidon cruise POS538 recovering the seismic streamer. (photo: Jonas Preine)
To create a structural image of the subsurface, sound waves are sent from the research vessel which travel through the subsurface and get reflected back at layer boundaries. This is known as a seismic profile and geophysicists use these to investigate structural interfaces in the subsurface. From their shape they reconstruct the geological processes and compare them with observations they make on land. They can tell for example if material has been torn apart or if it has been pushed together.
Maps of PRE-COLLAPSE case study volcanoes relevant in this Blog
