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Coalbed gas has been considered a hazard since the early 19th century when the first mine gas explosions occurred in the United States in 1810 and France in 1845. In eastern Australia methane-related mine disasters occurred late in the 19th century with hundreds of lives lost in New South Wales, and as recently as 1995 in Queensland's Bowen Basin.
This book arises from a two day international conference held at the Geological Society of London in November 1998. The meeting was organized with the purpose of bringing together sedimentologists, geomorphologists, archaeologists, environmental scientists and environmental managers to discuss recent research and topical issues relating to the interactions between natural processes, morphology and human activities in coastal and estuarine environments. More than 200 delegates, from 16 countries, attended the meeting over the course of the two days, stimulating lively discussion both about basic scientific issues and management implications. The meeting was sponsored by the British Sedimentological Research Group, the British Geomorphological Research Group, and English Heritage, and was also supported by the Environmental Sedimentology Committee of the International Association of Sedimentologists. The editors would like to thank these organizations, together with staff at the Geological Society and numerous daily helpers, especially postgraduate students and others from the University of Reading, for their generous assistance in making the meeting a great success
Interest in sediment dynamics is generated by the need to understand and predict: (i) morphodynamic and morphological changes, e.g. beach erosion, shifts in navigation channels, changes associated with resource development; (ii) the fate of contaminants in estuarine, coastal and shelf environment (sediments may act as sources
and sinks for toxic contaminants, depending upon the surrounding physico-chemical conditions); (iii) interactions with biota; and (iv) of particular relevance to the present Volume, interpretations of the stratigraphic record. Within this
context of the latter interest, coastal and shelf sediment may be regarded as a non-renewable resource; as such, their dynamics are of extreme importance. Over the years, various approaches and techniques have been applied to the determination of sediment transport pathways and the derivation of erosion, transport, and deposition rates. Such wide-ranging approaches include the refinement and application of numerical modelling; and the development of new and more efficient field equipment, e.g. video systems (coastal/ inshore) and multibeam. <...>
At the outset of this book, it is important to articulate clearly what we mean by ‘coast’, because the term means different things to different people. For most holidaymakers, the coast is synonymous with the beach. For birdwatchers, the coast generally refers to the intertidal zone; while for cartographers, the coast is simply a line on the map separating the land from the sea. Coastal scientists and managers tend to take a broader view.According to our perspective, the coast represents that region of the Earth’s surface that has been affected by coastal processes, i.e. waves and tides, during the Quaternary geological period (the last 2.6M years).
Here is the first complete manual on Coastal Geology. A book that gathers the knowledge of more than a century of research on different geological aspects of the coast: dynamics of geological processes, geomorphology, sedimentology and stratigraphy. They are also reflected from the applications of these sciences to the social problems and challenges of the communities occupying coastal areas. This manual collects many of my research experiences on different shores of the world, but almost everything written in this book I learned in other books.
Water resources are of enormous societal and ecological importance. In coastal areas, they are under ever greater pressure due to population growth, more affluent lifestyles, food production and the growing tourism industry. Changes to the coastal landscape, through urbanisation and land reclamation, and by natural processes such as climate change and sea level rise, modify the interaction between seawater and groundwater and put water resources at risk.
The COASTAL SEDIMENTS '07 conference was organized as a technical specialty conference devoted to the physical aspects of sediment processes and morphology change in the coastal and inlet environment. Following previous conferences in the Coastal Sediments series that were held in 1977, 1987, 1991, 1999, and 2003, COASTAL SEDIMENTS'07 celebrated 30 years of the Coastal Sediments series and promoted exchange of information and views among specialists in the fields of coastal engineering, geology, oceanography, and related disciplines. The theme of COASTAL SEDIMENTS
At first glance, coastal tectonics is as redundant a category as inland tectonics, for the shoreline does not necessarily coincide with a distinctive geodynamic environment. What prompted the international conference on the subject that led to this book was the Editors' conviction that coasts favour the study of active tectonics (a) by providing a reference datum- namely sea level- against which deformation can be measured and (b) by supplying datable material and environmental clues with which the progress of deformation can be traced <...>