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- W1994065637 abstract "The pre-transport environment of a coastal boulder along with its shape, size and density determines the height of wave required for it to be transported. Different forces act on sub-aerial boulders as opposed to submerged boulders when struck by a wave. Boulders derived from joint bounded blocks on shore platforms predominantly experience lift force and require a wave of greater height to be transported than boulders in other environments. No one equation is applicable to determine the height of palaeo-waves responsible for depositing a field or ridge of imbricated coastal boulders. A range of equations and their derivation is presented here which can be applied to the respective pre-transport environment of a boulder. Such an approach is necessary when attempting to reconstruct the frequency and magnitude of past coastal wave hazards and for differentiating between tsunami and storm wave deposited boulder fields." @default.
- W1994065637 created "2016-06-24" @default.
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- W1994065637 date "2003-05-01" @default.
- W1994065637 modified "2023-10-10" @default.
- W1994065637 title "Waves, coastal boulder deposits and the importance of the pre-transport setting" @default.
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- W1994065637 doi "https://doi.org/10.1016/s0012-821x(03)00104-3" @default.
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