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Fjords are glacially over-deepened, semi-enclosed marine basins, but are often neglected as a sedimentary realm. They represent the transition from the terrestrial to the marine environment and as such have the potential to preserve evidence of environmental change. Typically most fjords have been glaciated a number of times and some high-latitude fjords still possess a resident glacier. The stratigraphic record in fjords largely preserves a glacialdeglacial cycle of deposition. Sheltered water and high sedimentation rates potentially make fjords ideal depositional environments for preserving continuous records of climate and environmental change with high temporal resolution. Fjords are also referred to as miniature oceans providing the unique opportunity to study marine processes in great detail. With predictions of warming climates, changing ocean circulation and rising sea levels, this volume is a timely look at these environmentally sensitive coastlines.
The Geological Society of London
Founded in 1807, the Geological Society of London is the oldest geological society in the world, and one of the largest publishers in the Earth sciences.
The Society publishes a wide range of high-quality peer-reviewed titles for academics and professionals working in the geosciences, and enjoys an enviable international reputation for the quality of its work.
The many areas in which we publish in include:
-Petroleum geology
-Tectonics, structural geology and geodynamics
-Stratigraphy, sedimentology and paleontology
-Volcanology, magmatic studies and geochemistry
-Remote sensing
-History of geology
-Regional geology guides
- Sales Rank: #5507680 in Books
- Published on: 2011-01-15
- Original language: English
- Dimensions: 9.75" h x 7.00" w x 1.00" l, 2.05 pounds
- Binding: Hardcover
- 317 pages
Review
All together, I think that the book contains a wealth of interesting data and information. The various contributions reflect the recent advances and trends in modern fjord research, including the development and widespread application of new techniques for sea-floor mapping, as well as various proxies for the reconstruction of environmental and climate change. The results often show that fjords, frequently referred as a simple systems, are actually fairly complex. Despite several reviews, the book is not a complete and comprehensive fjord monograph, however, and several important fields - for instance biology and ecology - are underrepresented.
Many of the contributions to the book will be of interest for geologists and researchers in other disciplines (e.g. biology, ecology, climatology) working in modern fjord and estuarine environments. The book is also a valuable source of information for all the scientists engaged in climate and environmental palaeorecords. The combination of good review articles and high-quality multi-approach original studies makes the book useful, not only for active scientists but also for advanced students. --Witold Szczucinski - Adam Mickiewicz University, Poznan, Poland - Review featured in 'Geologos' , Tom van Loon book-review editor
........ essential reading for those interested in the post-LGM and Holocene climatic history of the fjords of Scotland and Svalbard, this multidisciplinary compilation has much to entice those interested in gaining a deeper insight into the past and future of these spectacular land-scape features. --Anna Hughes, Swansea University, UK - Featured in The Holocene March 2012
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