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- W2187713930 abstract "Inclined heterolithic stratification (IHS) forms the upper parts of a vegetated point-bar that forms the channel bank in the fluvial–tidal transition toward the head of the Severn Estuary. Continuing accretion of IHS occurs at the level of mean high water spring tides. The IHS overlies bar sands. The channel bank is convex upward with a tidal current-eroded scarp near the level of mean high water neap tides. At the foot of the scarp is a sandy bar reworked by tidal currents and weakly bioturbated by all but the lowest neap tides. The sandy bar is within the tidal channel and sections exhibit faint horizontal lamination with occasional ripple cross-lamination, mud flasers, reactivation surfaces, and convolutions. Convolutions are ascribed to pressure fluctuations due to tidal bores. In contrast, the IHS of the point-bar consists of distinctive thin laminations of sand, silt, and clay deposited by the higher spring tides. The channel bank top is inundated by slow currents, with little opportunity for reworking, which explains the preservation of distinctive IHS. The influence of high river discharge is not evident in the depositional signature, probably due to the intense mixing of high concentration estuarine suspended sediment in all weather and seasonal conditions." @default.
- W2187713930 created "2016-06-24" @default.
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- W2187713930 date "2015-01-01" @default.
- W2187713930 modified "2023-10-15" @default.
- W2187713930 title "Sedimentology of a tidal point-bar within the fluvial–tidal transition" @default.
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- W2187713930 doi "https://doi.org/10.1016/b978-0-444-63529-7.00008-0" @default.
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