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- W2010579622 abstract "Although the coasts of southern Ireland and eastern Nova Scotia possess many basic similarities, especially in terms of geology, glacial history, sediment character, resistance to erosion and wave and tide regimes, there is a fundamental contrast in Holocene sea-level history. In Ireland, recent (the past 4000 years) sea-level rise has been limited to less than 1 mm/year. By contrast, the Atlantic coast of Nova Scotia has been experiencing sea-level rises up to three to five times greater over the same period. Under these markedly differing relative sea-level rise regimes, barrier and lagoon evolution has varied considerably. In Ireland, barrier-lagoon form is controlled by local basement expression, particularly through the emergence of headlands (creating largely closed sediment systems) and the requirement to maintain cross-shore drainage. It is this latter factor that leads to a simple four-fold categorization of the Irish barriers and lagoons, from freshwater seepage to open tidal environments. The Nova Scotian examples are associated with rapidly moving erosional fronts, with local basement control relegated to a subordinate role at the expense of rapid changes in sediment supply. Barriers can both grow and decay under these conditions (subject to certain critical, but as yet ill-defined, thresholds), simultaneously forcing development and destruction of adjoining lagoons. These major differences also find expression in sedimentary sequences." @default.
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- W2010579622 date "1989-08-01" @default.
- W2010579622 modified "2023-09-26" @default.
- W2010579622 title "Barrier and lagoon coast evolution under differing relative sea-level regimes: examples from Ireland and Nova Scotia" @default.
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- W2010579622 doi "https://doi.org/10.1016/0025-3227(89)90099-6" @default.
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