Active Tectonics and Alluvial Rivers
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Product Description
The interactions between tectonic uplift, river erosion and alluvial deposition are fundamental processes which have acted to shape the landscape we see today. These processes are of course ongoing, and are important not only in geomorphology, sedimentology and structural geology, but also hydrology and river engineering. The authors have combined their specialities to bring together evidence and a variety of examples from both field and experimental studies to demonstrate how alluvial rivers are responding to uplift, subsidence and lateral tilting. Such recognition of the nature of river response yields criteria for the identification of active tectonics elsewhere, especially in areas without a history of seismic activity, or in the stratigraphic record. This volume will be of interest to graduate students, consultants and academic researchers in geomorphology, sedimentology and stratigraphy, structural geology, hydrology, geophysics and geography.
Product Details
- Amazon Sales Rank: #1370320 in Books
- Published on: 2002-02-21
- Original language: English
- Number of items: 1
- Dimensions: 1.02 pounds
- Binding: Paperback
- 292 pages
Editorial Reviews
Review
'… an important new contribution to tectonic geomorphology and fluvial geomorphology. The authors have done an excellent job of bringing together theory of river processes, field observation, experiment study, and synthesis to better understand the connections between active tectonics and river processes. The book will be of interest to a variety of people, including civil engineers, physical geographers, hydrologists, geologists, and ecologists … it is a really good read.' EOS
'This book brings together a large amount of literature and will be useful as a primer for engineers and earth scientists.' John Bridge, Sedimentology
'Find out how patterns of rivers may be used to trace movements of the Earth, from major faults such as the San Andreas to subtle uplifts such as the one along the Mississippi.' New Scientist
