Strand plain
In this article we are going to address the issue of Strand plain, which has been the subject of debate and analysis in various areas. Strand plain is a topic that arouses great interest and has generated different positions among experts and the general public. Throughout this article, we will thoroughly explore the relevant aspects related to Strand plain, as well as the implications it has in various contexts. We will focus on analyzing different approaches, recent research and perspectives that will help to more fully understand the importance and relevance of Strand plain today.
A strand plain or strandplain is a broad belt of sand along a shoreline with a surface exhibiting well-defined parallel or semi-parallel sand ridges separated by shallow swales. A strand plain differs from a barrier island in that it lacks either the lagoons or tidal marshes that separate a barrier island from the shoreline to which the strand plain is directly attached. Also, the tidal channels and inlets which cut through barrier islands are absent. Strand plains typically are created by the redistribution by waves and longshore currents of coarse sediment on either side of a river mouth. Thus, they are part of one type of wave-dominated delta.
Examples of strand plains:
- Western Louisiana
- Eastern Texas
- West coast of Namibia
- South-east and south-west coasts of Australia, and in the Gulf of Carpentaria
- Letea and Caraorman, Danube Delta, Romania
- Kustvlakte, Suriname
- Cayo Costa, Florida
See also
References
- ^ McCubbin, D.G., 1982, Barrier-island and strand-plain facies. in P.A. Scholle, and D. Spearing, eds., pp. 247–279., Sandstone Depositional Environments: Memoir no. 31, Tulsa, Oklahoma, American Association of Petroleum Geologists, Tulsa, Oklahoma.
- ^ Fitzgerald, D.M., W.J. Cleary, I.V. Buynevich, C.J. Hein, A.H.F. Klein, N. Asp, and R. Angulo, 2007, Strandplain Evolution along the Southern Coast of Santa Catarina, Brazil. Journal of Coastal Research. Supplemental issue no. 50, pp. 152-156.
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