Articles | Volume 22, issue 12
https://doi.org/10.5194/nhess-22-3939-2022
https://doi.org/10.5194/nhess-22-3939-2022
Research article
 | 
09 Dec 2022
Research article |  | 09 Dec 2022

Mass flows, turbidity currents and other hydrodynamic consequences of small and moderate earthquakes in the Sea of Marmara

Pierre Henry, M. Sinan Özeren, Nurettin Yakupoğlu, Ziyadin Çakir, Emmanuel de Saint-Léger, Olivier Desprez de Gésincourt, Anders Tengberg, Cristele Chevalier, Christos Papoutsellis, Nazmi Postacıoğlu, Uğur Dogan, Hayrullah Karabulut, Gülsen Uçarkuş, and M. Namık Çağatay

Viewed

Total article views: 2,765 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,896 770 99 2,765 225 47 54
  • HTML: 1,896
  • PDF: 770
  • XML: 99
  • Total: 2,765
  • Supplement: 225
  • BibTeX: 47
  • EndNote: 54
Views and downloads (calculated since 22 Nov 2021)
Cumulative views and downloads (calculated since 22 Nov 2021)

Viewed (geographical distribution)

Total article views: 2,765 (including HTML, PDF, and XML) Thereof 2,617 with geography defined and 148 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 02 Nov 2024
Download
Short summary
Seafloor instruments at the bottom of the Sea of Marmara recorded disturbances caused by earthquakes, addressing the minimum magnitude that may be recorded in the sediment. A magnitude 4.7 earthquake caused turbidity but little current. A magnitude 5.8 earthquake caused a mudflow and strong currents that spread sediment on the seafloor over several kilometers. However, most known earthquake deposits in the Sea of Marmara spread over larger zones and should correspond to larger earthquakes.
Altmetrics
Final-revised paper
Preprint