Sand waves
Sand waves under water in a shallow part of Gullmarn fjord

A sand wave is a lower regime sedimentary structure that forms across from tidal currents.[1]

Formation

Sand waves are formed through the action of the wind or water (through waves or tidal currents)[2] and are a product of unidirectional flow. Sand waves are the result of a mean flow velocity between 40 and 70cm/s.

Sand waves form also underwater.[3][4]

See also

References

  1. Allen, J.R.L. (1980). "Sand waves: A model of origin and internal structure". Sedimentary Geology. 26 (4): 281–328. Bibcode:1980SedG...26..281A. doi:10.1016/0037-0738(80)90022-6.
  2. Olsson-Seffer, Pehr Hjalmar (1910). Genesis and Development of Sand Formations on Marine Coasts. Augustana Book Concern, Printers. p. 17. Sand wave formed by winds.
  3. Pilkey, Orrin H. (2011-02-19). The World's Beaches: A Global Guide to the Science of the Shoreline. University of California Press. ISBN 978-0-520-26871-5.
  4. View toward San Francisco Bay of the massive sand wave field via ResearchGate.

Media related to Sand waves at Wikimedia Commons


This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.