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Submarine mass movements are a hidden geohazard with large destructive potential for submarine installations and coastal areas. This hazard and associated risk is growing in proportion with increasing population of coastal urban agglomerations, industrial infrastructure, and coastal tourism. Also, the intensified use of the seafloor for natural resource production, and deep sea cables constitutes an increasing risk. Submarine slides may alter the coastline and bear a high tsunamogenic potential. There is a potential link of submarine mass wasting with climate change, as submarine landslides can uncover and release large amounts greenhouse gases, mainly methane, that are now stored in marine sediments. The factors that govern the stability of submarine slopes against failure, the processes that lead to slope collapses and the collapse processes by themselves need to be better understood in order to foresee and prepare society for potentially hazardous events. This book volume consists of a collection of cutting edge scientific research by international experts in the field, covering geological, geophysical, engineering and environmental aspects of submarine slope failures. The focus is on understanding the full spectrum of challenges presented by this major coastal and offshore geohazard.
Recent global events such as the devastating 1998 Papua New Guinea tsunami, the 2004 Sumatran tsunami and the 2006 SE Asia undersea network cable failure underscore the societal and economic effects of submarine mass movements. These events call upon the scientific community to understand submarine mass movement processes and consequences to assist in hazard assessment, mitigation and planning. Additionally, submarine mass movements are beginning to be recognized as prevalent in continental margin geologic sections. As such, they represent a significant if not dominant role in margin sedimentary processes. They also represent a potential hazard to hydrocarbon exploration and development, but also represent exploration indicators and targets. This volume consists of a collection of the latest scientific research by international experts in geological, geophysical, engineering and environment aspects of submarine mass failures, focussed on understanding the full spectrum of challenges presented by submarine mass movements and their consequences.
Submarine mass movements represent major offshore geohazards due
to their destructive and tsunami-generation potential. This
potential poses a threat to human life as well as to coastal,
nearshore and offshore engineering structures. Recent examples of
catastrophic submarine landslide events that affected human
populations (including tsunamis) are numerous; e.g., Nice airport
in 1979, Papua-New Guinea in 1998, Stromboli in 2002, Finneidfjord
in 1996, and the 2006 and 2009 failures in the submarine cable
network around Taiwan. The Great East Japan Earthquake in March
2011 also generated submarine landslides that may have amplified
effects of the devastating tsunami. Given that 30% of the World 's
population live within 60 km of the coast, the hazard posed by
submarine landslides is expected to grow as global sea level rises.
This elevated awareness of the need for better understanding of
underwater landslides is coupled with great advances in underwater
mapping, sampling and monitoring technologies, laboratory analogue
and numerical modeling capabilities developed over the past two
decades. Multibeam sonar, 3D seismic reflection, and remote and
autonomous underwater vehicle technologies provide hitherto
unparalleled imagery of the geology beneath the oceans, permitting
investigation of submarine landslide deposits in great detail.
Increased and new access to drilling, coring, in situ measurements
and monitoring devices allows for ground-thruthing geophysical
data, provides access to samples for geotechnical laboratory
experiments and unprecedented in situ information on strength and
effective stress conditions of underwater slopes susceptible to
fail. Great advances in numerical simulation of submarine landslide
kinematics and tsunami propagation, particularly since the 2004
Sumatra tsunami, have also lead to increased understanding and
predictability of submarine landslide consequences.
Recent global events such as the devastating 1998 Papua New Guinea tsunami, the 2004 Sumatran tsunami and the 2006 SE Asia undersea network cable failure underscore the societal and economic effects of submarine mass movements. These events call upon the scientific community to understand submarine mass movement processes and consequences to assist in hazard assessment, mitigation and planning. Additionally, submarine mass movements are beginning to be recognized as prevalent in continental margin geologic sections. As such, they represent a significant if not dominant role in margin sedimentary processes. They also represent a potential hazard to hydrocarbon exploration and development, but also represent exploration indicators and targets. This volume consists of a collection of the latest scientific research by international experts in geological, geophysical, engineering and environment aspects of submarine mass failures, focussed on understanding the full spectrum of challenges presented by submarine mass movements and their consequences.
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