Geo-Marine Letters

, Volume 5, Issue 3, pp 171–176

Consequences of the El-Asnam earthquakes: Turbidity currents and slumps on the Algerian margin (Western Mediterranean)

  • M. El-Robrini
  • M. Gennesseaux
  • A. Mauffret
Article

DOI: 10.1007/BF02281635

Cite this article as:
El-Robrini, M., Gennesseaux, M. & Mauffret, A. Geo-Marine Letters (1985) 5: 171. doi:10.1007/BF02281635

Abstract

Seismicity due to the compressional motion in North Africa has an important effect on the stability of the sediments on the Algerian continental slope. The 1954 earthquake induced a large turbidity current that cut many telephone cables. Results of the 1980 El-Asnam earthquake on sliding of slope deposits arc not well documented, mainly because there were fewer cables than in the past. Nevertheless in the Bay of Alger, 200 km from the epicentre, a telephone cable was broken by a small turbidity current. This current reached a velocity of about 45 km/h.

Copyright information

© Springer-Verlag New York Inc. 1985

Authors and Affiliations

  • M. El-Robrini
    • 1
  • M. Gennesseaux
    • 1
  • A. Mauffret
    • 1
  1. 1.Département de Géologie DynamiqueUniversité Pierre et Marie CurieParis Cedex 05France