Subaqueous Mass Movements and their Consequences: Advances in Process Understanding, Monitoring and Hazard Assessments

This volume focuses on underwater or subaqueous landslides with the overarching goal of understanding how they affect society and the environment. The new research presented here is the result of significant advances made over recent years in directly monitoring submarine landslides, in standardizing global datasets for quantitative analysis, constructing a global database and from leading international research projects. Subaqueous Mass Movements demonstrates the breadth of investigation taking place into subaqueous landslides and shows that, while events like the recent ones in the Indonesian archipelago can be devastating, they are at the smaller end of what the Earth has experienced in the past. Understanding the spectrum of subaqueous landslide processes, and therefore the potential societal impact, requires research across all spatial and temporal scales. This volume delivers a compilation of state-of-the-art papers covering topics from regional landslide databases to advanced techniques for in situ measurements, to numerical modelling of processes and hazards.
The Last Glacial Maximum Balearic Abyssal Plain megabed revisited
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Published:June 11, 2020
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CiteCitation
Antonio Cattaneo, Shray Badhani, Cristina Caradonna, Massimo Bellucci, Estelle Leroux, Nathalie Babonneau, Sébastien Garziglia, Jeffrey Poort, Grigorii G. Akhmanov, Germain Bayon, Bernard Dennielou, Gwenäel Jouet, Sébastien Migeon, Marina Rabineau, Laurence Droz, Michael Clare, 2020. "The Last Glacial Maximum Balearic Abyssal Plain megabed revisited", Subaqueous Mass Movements and their Consequences: Advances in Process Understanding, Monitoring and Hazard Assessments, A. Georgiopoulou, L. A. Amy, S. Benetti, J. D. Chaytor, M. A. Clare, D. Gamboa, P. D. W. Haughton, J. Moernaut, J. J. Mountjoy
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Abstract
Megabeds are thick sedimentary layers extending over thousands of square kilometres in deep-sea basins and are thought to result from large slope failures triggered by major external events. Such deposits have been found in at least three areas of the Mediterranean Sea. Although their discovery dates back to the early 1980s, many questions remain concerning their initiation, source area, extent and the nature of their emplacement. One of the largest previously documented megabeds was emplaced during the Last Glacial Maximum across the Balearic Abyssal Plain, with a thickness of 8–10 m in water depths of up to 2800 m....
- abyssal plains
- Balearic Basin
- Cenozoic
- cores
- depositional environment
- erosion
- Europe
- facies
- failures
- geophysical methods
- geophysical profiles
- geophysical surveys
- Italy
- last glacial maximum
- lithofacies
- mechanical properties
- Mediterranean Sea
- ocean floors
- Pleistocene
- Quaternary
- Sardinia Italy
- seismic methods
- seismic profiles
- slope stability
- Southern Europe
- surveys
- thickness
- upper Pleistocene
- West Mediterranean