Results 161 to 170 of about 530 (214)
Numerical investigation of production performance of challenging gas hydrates from deposits with artificial fractures and impermeable barriers. [PDF]
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Reviews of Geophysics, 1996
Landslides are common on inclined areas of the seafloor, particularly in environments where weak geologic materials such as rapidly deposited, fine‐grained sediment or fractured rock are subjected to strong environmental stresses such as earthquakes, large storm waves, and high internal pore pressures.
Monty A. Hampton +2 more
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Landslides are common on inclined areas of the seafloor, particularly in environments where weak geologic materials such as rapidly deposited, fine‐grained sediment or fractured rock are subjected to strong environmental stresses such as earthquakes, large storm waves, and high internal pore pressures.
Monty A. Hampton +2 more
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Nature, 1998
Submarine landslides can generate enormous turbidity currents that carry that carry 500 km3or more of sediment down to the oceans' abyssal plains. The slides can cause Tsunamis, and may release large amounts of methane to the air.
Nisbet, Euan G., Piper, David J. W.
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Submarine landslides can generate enormous turbidity currents that carry that carry 500 km3or more of sediment down to the oceans' abyssal plains. The slides can cause Tsunamis, and may release large amounts of methane to the air.
Nisbet, Euan G., Piper, David J. W.
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Submarine landslides: advances and challenges
Canadian Geotechnical Journal, 2002Due to the recent development of well-integrated surveying techniques of the sea floor, significant improvements were achieved in mapping and describing the morphology and architecture of submarine mass movements. Except for the occurrence of turbidity currents, the aquatic environment (marine and fresh water) experiences the same type of mass failure
Jacques Locat, Homa J Lee
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Simulation of Submarine Landslides by Cellular Automata Methodology
2013A new model (named SCIDDICA-SS2), which is based on the Macroscopic Cellular Automata computational paradigm, has been specifically designed for the simula- tion of coastal and underwater landslides. SCIDDICA-SS2 is a fully 3D model based on the equivalent fluid approach.
Avolio M. V +4 more
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Submarine Landslides in French Polynesia
2004Landslides are common features of oceanic islands and playa key role in their evolution. Caused by caldera collapse or flank collapses, they can be classified into three types: (1) rock falls, (2) slumps or (3) debris avalanches (Moore et al. 1989). Rock falls, or superficial landslides, are mainly related to erosion processes of the subaerial parts of
Clouard, V., Bonneville, A.
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Submarine landslides: Elements of analysis
Marine Geotechnology, 1991The stability of seafloor sediments constitutes an important consideration in planning and design of various offshore facilities.
M. S. Rahman, W. Y. Jaber
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Determinants of Landslide Mobility and Landslide Area in Submarine Landslides
Artificial Intelligence and Applications / 794: Modelling, Identification and Control / 795: Parallel and Distributed Computing and Networks / 796: Software Engineering / 792: Web-based Education, 2013There are two central concepts in the analysis of mobility of landslides: the run-out distance which is defined as the horizontal distance between the initial centre of mass of the sliding material and the centre of mass of the sliding material subsequent to the landslide and the area which is defined as the total area affected by the landslide.
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Submarine Landslides and Tsunamis
20031. General Aspects of Tsunami Researches.- 1-1. Tsunamis of Seismic Origin Science, Disasters and Mitigation.- 1-2. Needs and Perspectives of Tsunami Research in Europe.- 2. Historical Tsunamis.- 2-1. Identification of Slide-generated Tsunamis in the Historical Catalogues.- 2-2. Updating and Revision of the European Tsunami Catalogue.- 2-3.
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Landslide‐modifications of submarine valleys
Eos, Transactions American Geophysical Union, 1932Introduction—The continental shelves are accordant in level to such a degree that they must have been remarkably free from earth‐movements both during and since their formation. Yet these same stable shelves are traversed in many places by deep elongate depressions many of which are so similar to river valleys that they have been attributed to the ...
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