The term “bedforms” is used for to describe rhythmic topographic features on the surface of granular beds. A wide variety of such features form in response to specific ranges of hydraulic conditions and grain size. Apart from their intrinsic scientific interest, bedforms are important in both geology and engineering. Large subaqueous bedforms can be obstacles to navigation, and their migration can be a threat to submarine structures. Bedforms also play an important role in determining the resistance to flow. Bedforms are also one of the most useful tools available for interpreting ancient sedimentary environments from outcrops.
When unidirectional flow operates on relatively fine-grained sand (less than 0.7 mm), the following bedforms appear in order as flow “strength” is increased: current ripples, dunes, upper-regime plane bed (absence of bedforms), antidunes, and cyclic steps. If the bed material is coarser than 0.7 mm, the ripple regime is replaced by lower-regime plane bed.
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Yokokawa, M. (2016). Bed forms. In: Harff, J., Meschede, M., Petersen, S., Thiede, J. (eds) Encyclopedia of Marine Geosciences. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-6238-1_141
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