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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
refutedsupported
the weight of evidence
5 sources for · 0 against

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.

Evidence for · 5
2019 · cited by 74
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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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.

More for · 4
2020 · cited by 33
Demonstrates that Holocene beach-ridge barriers on wave-dominated coastlines are fundamentally governed by sediment budget variations and sources.
2019 · cited by 14
Shows that sandy-shelly cheniers develop on mud-dominated wave-influenced coasts through the concentration and winnowing of coarse-grained bedload sediment supply.
2022 · cited by 1
Explicitly models how cheniers form through wave winnowing and onshore sand transport dependent on sediment supply and wave dynamics.
2022 · cited by 1
Explores the mechanisms of chenier formation through wave winnowing and sediment transport processes on coastal systems.
Everything we examined (12)
We also searched for evidence AGAINST this claim, not only for it.
  1. A starting guide to root ecology: strengthening ecological concepts and standardising root classification, sampling, processing and trait measurements.peer-reviewedno side takennot shown: read and judged not to bear on this claim
  2. The Materials Science behind Sustainable Metals and Alloys.peer-reviewedno side takennot shown: read and judged not to bear on this claim
  3. 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 changepeer-reviewedsupports
  4. What are the 100 most cited fungal genera?peer-reviewedno side takennot shown: read and judged not to bear on this claim
  5. Holocene evolution of the wave-dominated embayed Moruya coastline, southeastern Australia: Sediment sources, transport rates and alongshore interconnectivitypeer-reviewedsupports
  6. Multi-decadal Changes on the Mud-dominated Coast of Western French Guiana: Implications for Mesoscale Shoreline Mobility, River-mouth Deflection, and Sediment Sortingpeer-reviewedsupports
  7. Spatiotemporal Evolution of Coastal Dune Systems in the Çukurova Delta Plain: A Multitemporal Analysis Using Historical Aerial Photographs and UAV-Based Photogrammetrypeer-reviewedno side takennot shown: read and judged not to bear on this claim
  8. Sediment dynamics on a steep, megatidal, mixed sand-gravel-cobble beachpeer-reviewedno side takennot shown: read and judged not to bear on this claim
  9. Chenier Formation Through Wave Winnowing and Tidespeer-reviewedsupports
  10. Coastal evolution, environmental change and carbon storage in the Thung Prong Thong Mangrove, eastern Gulf of Thailandpeer-reviewedno side takennot shown: read and judged not to bear on this claim
  11. Chenier Formation Through Wave Winnowing and Tidal Transportpeer-reviewedsupports
  12. Advanced luminescence dating of the Karapürçek formation reveals middle pleistocene tectonic reorganization of the North Anatolian Fault Zone.peer-reviewedno side takennot shown: read and judged not to bear on this claim
The paper trail · every fact has a biography
first checked05 Aug 2026
judged → SUPPORTED · 8705 Aug 2026
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