Abstract
Beach processes and, in a broader sense also coastal and shelf processes, are controlled predominantly by wind waves, tidal waves, and wave-generated currents. In this first chapter on coastal and shelf sediments we shall briefly discuss wind waves and wind-generated currents of the coastal zone (wave-dominated shorelines). Detailed descriptions of these processes have been given in several books, recently for example by Carter (1988). Tidal effects and other oceanic currents will be referred to in Chapters 3.2 and 3.3.
Keywords
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.
This is a preview of subscription content, log in via an institution.
Buying options
Tax calculation will be finalised at checkout
Purchases are for personal use only
Learn about institutional subscriptionsPreview
Unable to display preview. Download preview PDF.
Author information
Authors and Affiliations
Rights and permissions
Copyright information
© 1992 Springer-Verlag Berlin Heidelberg
About this chapter
Cite this chapter
Einsele, G. (1992). Coastal and Shallow Sea Sediments (Including Carbonates). In: Sedimentary Basins. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-77055-5_3
Download citation
DOI: https://doi.org/10.1007/978-3-642-77055-5_3
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-540-54449-4
Online ISBN: 978-3-642-77055-5
eBook Packages: Springer Book Archive