Svend Saxov and J.K. Nieuwenhuis Laboratory of Geophysics, Aarhus University Finlandsgade 6, DK-8200 Aarhus N, Denmark Ministry of Transport and Public Works Rijkswaterstaat, Deltadienst Van Alkemadelaan 400, 2597 AT the Hague The Netherlands The NATO Science Committee Special Programme Panel on Marine Sciences decided in September 1979 that a work ing group should prepare a document dealing with the prob lems of marine slides. The working group submitted to the Panel a proposal for the arrangement of an interdisciplinary workshop on Marine Slides and other Mass Movements, and the Panel decided to fund such a workshop. Mass movement of soils and rocks on subaerial slopes is a subject which has been intensely studied over the past fifty years, and its literature is becoming extens ive. The submarine phenomenon, although similar in its pbysical basis, is much less studied, but has become an important subject (particularly during the past decade) because of the increase of man's use of the coastal en vironment and the intensified exploration for oil and minerals on the continental margins and ocean basins.

Klappentext

Svend Saxov* and J.K. Nieuwenhuis** *Laboratory of Geophysics, Aarhus University Finlandsgade 6, DK-8200 Aarhus N, Denmark **Ministry of Transport and Public Works Rijkswaterstaat, Deltadienst Van Alkemadelaan 400, 2597 AT the Hague The Netherlands The NATO Science Committee Special Programme Panel on Marine Sciences decided in September 1979 that a work­ ing group should prepare a document dealing with the prob­ lems of marine slides. The working group submitted to the Panel a proposal for the arrangement of an interdisciplinary workshop on Marine Slides and other Mass Movements, and the Panel decided to fund such a workshop. Mass movement of soils and rocks on subaerial slopes is a subject which has been intensely studied over the past fifty years, and its literature is becoming extens­ ive. The submarine phenomenon, although similar in its pbysical basis, is much less studied, but has become an important subject (particularly during the past decade) because of the increase of man's use of the coastal en­ vironment and the intensified exploration for oil and minerals on the continental margins and ocean basins.

Inhalt
Marine Slides Some Introductory Remarks.- Geology and Geodynamical Settings.- On the Tectonic Setting of Submarine Slides.- Active Slides and Flows in Underconsolidated Marine Sediments on the Slopes of the Mississippi Delta.- Coastal Geomorphology.- Recent Mass Wasting Processes on the Provencal Margin (Western Mediterranean).- Mechanics of Marine Slides and Other Mass Movements.- Some Aspects of Submarine Slope Stability.- On an Explanation of Marine Flow Slides in Sand.- Submarine Slumping and Mass Movements on the Continental Slope of Israel.- Piezometer Probes for Assessing Effective Stress and Stability in Submarine Sediments.- Marine Slope Stability A Geological Approach.- Geophysics.- Imaging of Submarine Landslides with Wide-Swath Sonar.- Anatomy of Some Atlantic Margin Sediment Slides and Some Comments on Ages and Mechanisms.- Evidences of Late Quaternary Mass Movements in the Bay of Biscay.- Earthquake Seismology.- Estimation of Earthquake Ground Motions Relevant to the Triggering of Marine Mass Movements.- Tsunami as Triggering Mechanism of Homogenites Recorded in Areas of the Eastern Mediterranean Characterized by the Cobblestone Topography.- Oceanography.- Interrelationships between Oceanographic Events and Mass Wasting of the Sea Floor.- Marine Sedimentaology.- The Deposition of Thin Bedded Subaqeous Debris Flow Deposits.- Long-Range Sidescan Sonar Studies of Sediment Slides and the Effects of Slope Mass Sediment Movement on Abyssal Plain Sedimentaion.- Unusual Debris Flow Deposits from the Base of the Malta Escarpment (Eastern Mediterranean).- Marine Biology.- Marine Slides and Allopatric Speciation.- Possible Benthic Fauna and Slope Instability Relationships.- Discussion, Summary and Recommendation.