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Seabed Seismographs Reveal Duration and Structure of Longest Runout Sediment Flows on Earth

Baker, Megan L.; Talling, Peter J.; Burnett, Richard; Pope, Ed L.; Ruffell, Sean C.; Urlaub, Morelia; Clare, Michael A.; Jenkins, Jennifer; Dietze, Michael; Neasham, Jeffrey; Silva Jacinto, Ricardo; Hage, Sophie; Hasenhündl, Martin; Simmons, Steve M.; Heerema, Catharina J.; Heijnen, Maarten S.; Kunath, Pascal; Cartigny, Matthieu J. B.; McGhee, Claire; Parsons, Daniel R.

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Authors

Richard Burnett

Profile image of Sean Ruffell

Sean Ruffell sean.ruffell@durham.ac.uk
PGR Student Doctor of Philosophy

Morelia Urlaub

Michael A. Clare

Michael Dietze

Jeffrey Neasham

Ricardo Silva Jacinto

Sophie Hage

Martin Hasenhündl

Steve M. Simmons

Catharina J. Heerema

Maarten S. Heijnen

Pascal Kunath

Claire McGhee

Daniel R. Parsons



Abstract

Turbidity currents carve the deepest canyons on Earth, deposit its largest sediment accumulations, and break seabed telecommunication cables. Powerful canyon‐flushing turbidity currents break sensors placed in their path, making them notoriously challenging to measure, and thus poorly understood. This study provides the first remote measurements of canyon‐flushing flows, using ocean‐bottom seismographs located outside the flow's destructive path, revolutionizing flow monitoring. We recorded the internal dynamics of the longest sediment flows yet monitored on Earth, which traveled >1,000 km down the Congo Canyon‐Channel at 3.7–7.6 m s−1 and lasted >3 weeks. These observations allow us to test fundamental models for turbidity current behavior and reveal that flows contain dense and fast frontal‐zones up to ∼400 km in length. These frontal‐zones developed near‐uniform durations and speeds for hundreds of kilometres despite substantial seabed erosion, enabling flows to rapidly transport prodigious volumes of organic carbon, sediment, and warm water to the deep‐sea.

Citation

Baker, M. L., Talling, P. J., Burnett, R., Pope, E. L., Ruffell, S. C., Urlaub, M., Clare, M. A., Jenkins, J., Dietze, M., Neasham, J., Silva Jacinto, R., Hage, S., Hasenhündl, M., Simmons, S. M., Heerema, C. J., Heijnen, M. S., Kunath, P., Cartigny, M. J. B., McGhee, C., & Parsons, D. R. (2024). Seabed Seismographs Reveal Duration and Structure of Longest Runout Sediment Flows on Earth. Geophysical Research Letters, 51(23), Article e2024GL111078. https://doi.org/10.1029/2024gl111078

Journal Article Type Letter
Acceptance Date Nov 6, 2024
Online Publication Date Nov 28, 2024
Publication Date Dec 16, 2024
Deposit Date Dec 2, 2024
Publicly Available Date Dec 2, 2024
Journal Geophysical Research Letters
Print ISSN 0094-8276
Electronic ISSN 1944-8007
Publisher Wiley
Peer Reviewed Peer Reviewed
Volume 51
Issue 23
Article Number e2024GL111078
DOI https://doi.org/10.1029/2024gl111078
Keywords organic carbon, ocean‐bottom seismographs, ocean fluxes, seismic monitoring, turbidity currents
Public URL https://durham-repository.worktribe.com/output/3115977

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