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Subaqueous mass movements include landslides, debris flows and turbidity currents. Their far-reaching impacts threaten densely-populated coastal regions, global economies and the environment. They have the potential to generate devastating tsunamis, severely damage seafloor infrastructure and transport vast amounts of sediment and microplastics to the ocean floor. They also play an important role in the deep sea burial of organic carbon.

Although often compared to their subaerial counterparts, run-out distances of subaqueous mass movements may be substantially greater (hundreds of kilometres), and can occur at remarkably lower gradients (

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Convener: Davide MencaroniECSECS | Co-conveners: Shray BadhaniECSECS, Kate HeeremaECSECS, Maarten HeijnenECSECS, William MeservyECSECS
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| Attendance Mon, 04 May, 16:15–18:00 (CEST)

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Chat time: Monday, 4 May 2020, 16:15–18:00

EGU2020-3194
Tectonic and geomorphic controls on the distribution of submarine landslides across active and passive margins, eastern New Zealand
Sally Watson et al.
EGU2020-12140
Insights into potential submarine landslide tsunamis in the South China Sea: A comparative study of the Baiyun Slide and the Brunei Slide
Linlin Li et al.
EGU2020-8826
Diffraction imaging to understand the internal fabric of mass-transport complexes from Gulf of Cadiz, south west Iberian Margin
Jonathan Ford et al.
EGU2020-163
Fluid flow and pore pressure development throughout the evolution of a trough mouth fan and implications for the slope stability, western Barents Sea
Jaume Llopart et al.
EGU2020-2578
Seismic strengthening of diatom-rich sediments: A comparison of slope sediments from Chilean lakes and the Japan Trench margin
Jasper Moernaut et al.
EGU2020-6979
Stability assessment of submerged lateral and deltaic slopes in Lake Lucerne
Anastasiia Shynkarenko et al.
EGU2020-20168
A new mechanism for the triggering of turbidity currents offshore tropical river deltas
Gaetano Porcile et al.
EGU2020-18904
How deep does sand deposits in the Alentejo basin (Gulf of Cadiz) reach? Evaluating slope stability from bottom-current activities through time
Davide Mencaroni et al.
EGU2020-19658
Imaging seafloor instabilities using very high-resolution deep-towed multichannel seismic data in the Gulf of Lions (NW Mediterranean)
Shray Badhani et al.
EGU2020-18710
Why is the Tuaheni Landslide Complex a spreading failure?
Morelia Urlaub et al.
EGU2020-5841
Late Quaternary Tectonics vs Sedimentation history of the offshore Termini in a seismically active segment of the Northern Sicily Continental margin (Southern Tyrrhenian Sea)
Elisabetta Zizzo et al.
EGU2020-9031
Submarine landslide recurrence and links to seismicity on the Gorringe Bank Seamount, Offshore Portugal
Davide Gamboa et al.
EGU2020-11327
Geotechnical properties of marine sediments in the SW Iberia Margin – Implications to marine geohazards.
Aldina Piedade et al.
EGU2020-14056
Sharp changes in lake-levels preconditioning seismogenic mass failures in the Dead Sea
Yin Lu et al.
EGU2020-19799
Bayesian back analysis for dynamic CPTu strain-rate correction.
Stefano Collico et al.
EGU2020-15909
Sediment failure of St. Pierre Slope: new insights of failure mechanisms and slope instability due to the 1929 Grand Banks Earthquake
Irena Schulten et al.
EGU2020-7973
Characterization of recent deep-sea debrites in the Eastern Mediterranean based on foraminiferal taphonomy
Oded Katz et al.
EGU2020-10289
Slow build-up of turbid currents triggered by a moderate earthquake in the Sea of Marmara
Pierre Henry et al.
EGU2020-21034
Testing the veracity of turbidite paleoseismology using the Kaikōura earthquake-triggered turbidite, New Zealand
not presented
Alan Orpin et al.
EGU2020-2407
First direct monitoring and time-lapse mapping starts to reveal how a large submarine fan works | Highlight
Peter Talling et al.