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.
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.