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Showing 1 to 1 of 1 for “"Ostend Valley"”.
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The Quaternary geological evolution of the Belgian Continental Shelf, southern North Sea
… Three basal units (U1, U2, U3) infill a large valley, incised during the Saalian ice-age in the Top-Paleogene (former Top-Tertiary) surface, i.e. the Ostend Valley. The three units, separated by tidal ravinement surfaces, represent successive phases of a transgressive estuarine infilling during …