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• W1991523788 abstract "The retreat of the macrotidal Severn Estuary inland up the Severn Vale, under the drive of a rising relative sea level, is demonstrated by (1) the erosion of marginal bedrock cliffs, (2) the present-day wide intertidal exposure of mid post-glacial rooted peats formed on early tidal marshes, (3) the transposition into post-settlement deposits and the present-day intertidal zone of prehistoric and early historic cultural debris representing wetland exploitation, and (4) the erosive relationship between modem sand-flat deposits and the older post-glacial silts and clays. A consideration of the sources, stores and pathways of fine sediment suggests, on a balance of evidence, that the system has recently reached its maximum capacity, and has for a substantial period been retreating inland by a “roll-over” process involving the reworking of long-deposited fine sediments into active environments. The export of fine sediment to the continental shelf could now be taking place." @default.
• W1991523788 created "2016-06-24" @default.
• W1991523788 creator A5005277423 @default.
• W1991523788 date "1990-02-01" @default.
• W1991523788 modified "2023-10-15" @default.
• W1991523788 title "The Severn Estuary in southwest Britain: its retreat under marine transgression, and fine-sediment regime" @default.
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• W1991523788 doi "https://doi.org/10.1016/0037-0738(90)90003-c" @default.
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