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the claim

Chenier ridges and strand plains form through sediment supply variations at wave-dominated coastlines

the verdict
SUPPORTED
the evidence backs this
Recorded sources
5 sources for · 0 against

Counts group repeated records of the same source within each side. They do not measure evidence strength or source independence.

Is it true that Chenier ridges and strand plains form through sediment supply variations at wave-dominated coastlines?

Yes. Multiple coastal and geomorphological studies confirm that the formation of chenier ridges and strand plains on wave-dominated coastlines is driven by fluctuations and variations in sediment supply and wave-driven winnowing processes.

Verdict: SUPPORTED · 5 sources for, 0 against · Last checked

The analysis

Papers [2], [4], [5], [8], and [10] provide strong empirical and numerical modeling evidence demonstrating how cheniers and strand plains (such as beach-ridge barriers) form on wave-dominated coasts as a direct result of sediment supply dynamics, sand availability, and wave-induced winnowing. There is no contradictory evidence in the provided literature regarding this geological process.

Evidence for · 5
Response of the Bight of Benin (Gulf of Guinea, West Africa) coastline to anthropogenic and natural forcing, Part 2: Sources and patterns of sediment supply, sediment cells, and recent shoreline change
2019
Identifies variations in sediment supply along wave-dominated coastlines as key drivers for shoreline change, barrier stability, and beach-ridge formation.
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Anthony, E., Almar, R., Besset, M., Reyns, J., Laibi, R., Ranasinghe, R., Ondoa, G. A., & Vacchi, M. (2019). Response of the Bight of Benin (Gulf of Guinea, West Africa) coastline to anthropogenic and natural forcing, Part 2: Sources and patterns of sediment supply, sediment cells, and recent shoreline change. doi.org. https://doi.org/10.1016/J.CSR.2018.12.006

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More for · 4
Holocene evolution of the wave-dominated embayed Moruya coastline, southeastern Australia: Sediment sources, transport rates and alongshore interconnectivity
2020
Demonstrates that Holocene beach-ridge barriers on wave-dominated coastlines are fundamentally governed by sediment budget variations and sources.
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Oliver, T., Tamura, T., Brooke, B., Short, A., Kinsela, M., Woodroffe, C., & Thom, B. (2020). Holocene evolution of the wave-dominated embayed Moruya coastline, southeastern Australia: Sediment sources, transport rates and alongshore interconnectivity. doi.org. https://doi.org/10.1016/j.quascirev.2020.106566

Multi-decadal Changes on the Mud-dominated Coast of Western French Guiana: Implications for Mesoscale Shoreline Mobility, River-mouth Deflection, and Sediment Sorting
2019
Shows that sandy-shelly cheniers develop on mud-dominated wave-influenced coasts through the concentration and winnowing of coarse-grained bedload sediment supply.
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Jolivet, M., Gardel, A., & Anthony, E. (2019). Multi-decadal Changes on the Mud-dominated Coast of Western French Guiana: Implications for Mesoscale Shoreline Mobility, River-mouth Deflection, and Sediment Sorting. doi.org. https://doi.org/10.2112/SI88-014.1

Chenier Formation Through Wave Winnowing and Tides
2022
Explicitly models how cheniers form through wave winnowing and onshore sand transport dependent on sediment supply and wave dynamics.
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Tas, S., Maren, D. V. v., & Reniers, A. (2022). Chenier Formation Through Wave Winnowing and Tides. doi.org. https://doi.org/10.1029/2022JF006792

Chenier Formation Through Wave Winnowing and Tidal Transport
2022
Explores the mechanisms of chenier formation through wave winnowing and sediment transport processes on coastal systems.
Get citation
Tas, S., Maren, B. v., & Reniers, A. (2022). Chenier Formation Through Wave Winnowing and Tidal Transport. doi.org. https://doi.org/10.1002/essoar.10511574.1

Receipt History
first checked05 Aug 2026
judged → SUPPORTED · 8705 Aug 2026
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