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Fig. 1 | Progress in Earth and Planetary Science

Fig. 1

From: Reconstruction of sediment-transport pathways on a modern microtidal coast by a new grain-size trend analysis method

Fig. 1

Index map showing locality of the study area. The data of the residual current velocity (in a) are from the Coastal Oceanography Research Committee, The Oceanographic Society of Japan (1985). ‘R’ and ‘W’ (in a) are measurement localities of rainfall and water depth, respectively. Data are from the Japan Meteorological Agency (JMA) (see Fig. 10; Details of the geomorphological features of the study area (dotted line in b) are described in Fig. 2

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