Authors

Abigail Metcalfe, Laboratoire Magmas et Volcans, Clermont-Ferrand
Katharina Pank, Helmholtz Centre for Ocean Research Kiel
Steffen Kutterolf, Helmholtz Centre for Ocean Research Kiel
Jonas Preine, Woods Hole Oceanographic Institution
Paraskevi Nomikou, National and Kapodistrian University of Athens
Christian Hübscher, University of Hamburg
Thomas A. Ronge, Alfred Wegener Institute - Helmholtz Centre for Polar and Marine Research
Sarah Beethe, Oregon State University
A Bernard
Carole Berthod, CNRS
Hehe Chen, China University of Geosciences, Beijing
Shun Chiyonobu, Akita University
Acacia Clark, University of Tasmania
Susan DeBari, Western Washington University
Tatiana Fernandez-Perez, Kent State University
Ralf Gertisser, Keele University
Christopher Jones, University of California at Riverside
Raymond Johnston, University of South Florida
Kumar Batuk Joshi, National Centre for Earth Science Studies
Jens Karstens, Helmholtz Centre for Ocean Research Kiel
Günther Kletetschka, University of Alaska Fairbanks
Olga Koukousioura, Aristotle University of Thessaloniki
Hao Yang Lee, Academia Sinica - Institute of Earth Sciences
Xiaohui Li, Guangdong Enterprise Key Laboratory for Urban Sensing
Michael Manga, University of California at Berkeley
Molly McCanta, Tufts University
Iona McIntosh, Japan Agency for Marine-Earth Science and Technology
Tony Morris, School of Geography, Earth and Environmental Sciences
Dimitrios Papanikolaou, National and Kapodistrian University of Athens
Ally Peccia, Columbia University

ORCID

Abstract

The histories of submarine explosive volcanoes are commonly poorly known due to inaccessibility of their eruptive archives. This raises uncertainties in the eruption frequencies of these highly hazardous systems, and in their interactions with neighboring volcanoes. The submarine Kolumbo Volcanic Chain (KVC) northeast of Santorini is made up of the polygenetic Kolumbo Volcano and a linear zone of more than 20 smaller volcanic cones and is one of the most active eruptive centers on the South Aegean Volcanic Arc. However, despite the destructive eruption of Kolumbo in 1650 CE, and unrest in 2024–2025, the eruptive history of the KVC is poorly known. International Ocean Discovery Program (IODP) Expedition 398 deep-drilled the seafloor at two sites on the western flank of Kolumbo. Here, we use tephrostratigraphy to identify 19 explosive eruptions of the KVC (probably mostly Kolumbo itself) ranging from basaltic andesite to rhyolite in composition and beginning at ca. 265 ka. The lifespan-averaged recurrence time of explosive activity along the KVC is ~6 k.y. (but as low as ~1 k.y. between 178 ka and 164 ka), although many of these eruptions were smaller than that of 1650 CE. The birth of Kolumbo coincided with the transition of Santorini to highly explosive activity, possibly due to joint interactions with regional lithospheric stresses. Moreover, the three main phases of edifice construction at Kolumbo (ca. 265–193 ka, 24 ka, and 0.4 ka) broadly correspond to periods of caldera-forming eruptions at Santorini, reflecting additional couplings between the two volcanic systems on shorter time scales.

Publication Date

2026-02-02

Publication Title

Geology

ISSN

0091-7613

Acceptance Date

2026-01-09

Deposit Date

2026-02-24

Creative Commons License

Creative Commons Attribution 4.0 International License
This work is licensed under a Creative Commons Attribution 4.0 International License.

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