Английская Википедия:Baymouth bar

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Шаблон:Short description Шаблон:Multiple issues Шаблон:Use mdy dates A baymouth bar is a depositional feature as a result of longshore drift. It is a sandbank that partially or completely closes access to a bay.[1]

Background

These bars usually consist of accumulated gravel and sand carried by the current of longshore drift and deposited at a less turbulent part of the current. Thus, they most commonly occur across artificial bay and river entrances due to the loss of kinetic energy in the current after wave refraction.Шаблон:Cn

References

Шаблон:Reflist Шаблон:Coastal geography


Шаблон:Marine-geo-stub