Last Updated:2025/12/07

Coastal currents can sedimentize suspended silt, gradually building up barrier islands over centuries.

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Coastal currents can sedimentize suspended silt, gradually building up barrier islands over centuries.

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沿岸の海流は懸濁したシルトを沈殿させ、何世紀にもわたって徐々に砂州を形成することがある。

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