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Point Futtsu is the cuspate foreland separating Tokyo Bay and the Uraga Strait. In recent years, the shoreline around this cuspate foreland is considered to be stable, but large-scale seasonal variation may occur because wave direction at the tip of the cuspate foreland reverses seasonally. In the previous studies, however, such seasonal variation in beach topography has not been studied. We measured the seasonal variation of the shoreline configuration around the tip of the sand spit and the topographic response to incident waves was investigated by field observation. A large sand spit formed before June 11, 2011 was markedly deformed due to the action of predominant waves incident from the direction of NNW in Tokyo Bay. This sand spit was assumed to be formed by the action of the 2011 Great Tsunami.

Field Observation of Large-scale Seasonal Variation of Sand Spit at Tip of Point Futtsu