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On the minimum amplitude of regional sea-level fluctuations during the Flandrian

✍ Scribed by J. R. L. Allen


Publisher
John Wiley and Sons
Year
1997
Tongue
English
Weight
72 KB
Volume
12
Category
Article
ISSN
0267-8179

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✦ Synopsis


The mathematical form of a time-height sea-level curve representing intermediatefrequency fluctuations superimposed on an underlying upward trend yields a simple method for estimating the minimum amplitude of fluctuations from field measurements of the thickness of silt-peat couplets. Drawing on data from the Thames Estuary and the Fenland Basin, fluctuations of relative sea-level with minimum amplitudes between 0.08 m and 0.91 m seem to have occurred in the southeast British region during the mid-Flandrian.