Abstract

The development process of the Hamamatsu strand plain was studied by using Optically Stimulated Luminescence (OSL) dating. The temporal and spatial change of Enshu-nada coast line for 6000 years was revealed by the OSL ages of feldspar partides in foreshore sediments under beach ridges. The rate of coastal progradation was estimated at 1.06 m/year within 1500 years. The speed corresponds quantitatively with the estimation of previous studies.

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