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Chenier or Chénier is a sandy or shelly beach ridge that is part of a strand plain, called a “chenier plain,” consisting of cheniers separated by intervening mud-flat deposits with marsh and swamp vegetation. Cheniers are typically 1 to 6 m high, tens of km long, hundreds of metres wide, and often wooded. Chenier plains can be tens of km wide. Cheniers and associated chenier plains are associated with shorelines characterized by generally low wave energy, low gradient, muddy shorelines, and abundant sediment supply. The name is derived from the French word for wood, “chêne,” meaning oak, which grows on chenier ridges within southwest Louisiana.[1][2]

Cheniers made primarily of shells of the Colorado Delta clam are found in the tidal flats of the Colorado River Delta in northeastern Baja California, Mexico, as well as in Essex, England.[3][4] In Essex, Ground-truthing data demonstrate that the radar profiles accurately delineate the subsurface stratigraphy and sedimentary structure of the cheniers. Interpretation of the radar stratigraphy taken from the radar reflection profiles allows various deposits to be identified. These have resulted from overwashing, overtopping, sedimentation across the whole of a seaward dipping beachface or berm ridge welding onto the upper beachface. Each chenier is characterised by a different spatial arrangement of these four basic depositional units.[4]


The Louisiana Chenier Plain, extending roughly from Sabine Lake to Vermilion Bay along the Gulf Coast, serves critical ecosystem functions, particularly as a wildlife habitat and stopover for migrating birds. As the region was settled, the cheniers were developed preferentially, owing to protection from flooding afforded by the higher elevation. Examples of communities situated on such ridges in the Chenier Plain include Grand Chenier in Cameron Parish, Pecan Island in Vermilion Parish and the former settlement of Cheniere Caminada adjacent to Grand Isle, south of New Orleans. The ridges, however, offer insufficient protection from storm surges, thus Cheniere Caminada was completely destroyed by a hurricane in 1893, and Pecan Island and Grand Chenier have been devastated by several powerful storms, including Hurricane Audrey, Hurricane Rita, and Hurricane Ike.

Kirby[5] explains how sediment deposition through the null point hypothesis leads to the creation of chenier. Sediment fines are suspended and reworked aerially offshore leaving behind lag deposits of mainly bivalve and gastropod shells separated out from the finer substrate beneath, waves and currents then heap these deposits to form chenier ridges throughout the tidal zone which tend to be forced up the foreshore profile but also along the foreshore.

New Zealand[edit]

The chenier plain in Miranda is one of the most significant Holocene coastal strand plains in the world and an important stopover point in the godwit flightpath. [1]


  1. ^ Goodie, A.S. (2004) Encyclopedia of Geomorphology Routledge. London, United Kingdom. 1,200 p. ISBN 978-0-415-32738-1
  2. ^ Otvos, E.G. and W.A. Price (1979) Problems of chenier genesis and terminology—an overview. Marine Geology. v. 31, pp. 251–263.
  3. ^ Kowalewski, M., and K.W. Flessa (1995) Comparative taphonomy and faunal composition of shelly cheniers from northeastern Baja California, Mexico. Archived August 26, 2010, at the Wayback Machine. Ciencias Marinas. v. 21, no. 2, pp. 155-177.
  4. ^ a b Neal, A.R.J., and K. Pye (2002) Structure and development of shell cheniers in Essex, southeast England, investigated using high frequency ground-penetrating radar. Marine Geology. v. 185, pp. 435-469.
  5. ^ Kirby R. (2002). Distinguishing accretion from erosion-dominated muddy coasts. In T. W. Healy, Y. and Healy J. (Ed.), Muddy coasts of the world:Processes, deposits and function. Elsevier. pp. 61–81). 

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