Scientific Drilling
Scientific Drilling
SD
Articles | Volume 32
Articles | Volume 32
https://doi.org/10.5194/sd-32-27-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/sd-32-27-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 32
Science report
 | 
26 Oct 2023
Science report |  | 26 Oct 2023

Drilling into a deep buried valley (ICDP DOVE): a 252 m long sediment succession from a glacial overdeepening in northwestern Switzerland

Sebastian Schaller, Marius W. Buechi, Bennet Schuster, and Flavio S. Anselmetti

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Cited articles

Alley, R. B., Cuffey, K. M., and Zoet, L. K.: Glacial erosion: status and outlook, Ann. Glaciol., 60, 1–13, https://doi.org/10.1017/aog.2019.38, 2019. 
Anselmetti, F. S., Bavec, M., Crouzet, C., Fiebig, M., Gabriel, G., Preusser, F., Ravazzi, C., and DOVE scientific team​​​​​​​: Drilling Overdeepened Alpine Valleys (ICDP-DOVE): quantifying the age, extent, and environmental impact of Alpine glaciations, Sci. Dril., 31, 51–70, https://doi.org/10.5194/sd-31-51-2022, 2022. 
Bouma, A. H.: Sedimentology of some Flysch deposits: a graphic approach to facies interpretation, Elsevier, Amsterdam, the Netherlands, https://lib.ugent.be/catalog/rug01:000978747 (last access: 21 September 2023), 1962. 
Brandt, A. C.: Erkundung des alpinen, glazial-übertieften Basadingen-Beckens mithilfe von P-Wellen-Seismik, BSc thesis, Leibniz Universität Hannover, unpublished, 2020. 
Buechi, M. W., Frank, S. M., Graf, H. R., Menzies, J., and Anselmetti, F. S.: Subglacial emplacement of tills and meltwater deposits at the base of overdeepened bedrock troughs, Sedimentology, 64, 658–685, https://doi.org/10.1111/sed.12319, 2017. 
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Short summary
In the frame of the DOVE (Drilling Overdeepened Alpine Valleys) project and with the support of the International Continental Scientific Drilling Program (ICDP), we drilled and recovered a 252 m long sediment core from the Basadingen Through. The Basadingen Trough, once eroded by the Rhine glacier during several ice ages, reaches over 300 m under the modern landscape. The sedimentary filling represents a precious scientific archive for understanding and reconstructing past glaciations.
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