Kumano Ura Beach which extends about 25km long and 100m wide from Kumano City to Shingu City affords an ideal laboratory for a study of the processes of transportation and deposition on beach sediments. Samples of beach sediments collected are parallel and normal to the shore. These samples were analyzed in order to determine their size distribution and properties of roundness and shape. Conclusions drawn from this study are as follows:
(1) Grain size shows a certain marked variation with changing wave condition on a beach. Generally, beach sediments show tonal distribution with finer and coarser part. Thus the grainsorting was influ enced by the differences between the action of the surf and backwash.
(2) Beach sediments between 8 and 2mm tend to become rounded by abrasion during transportation. This fact does not agree to the results of work reported in other studies of river transported sediments. Itt is presumably the results of the rubbing of fine material as they roll over each other without the resistante of water.
(3) On a foreshore beach pebbles show more evidence of sorting according to shape for spheroidal and ellipsoidal pebbles deposit on the place where waves reach and flat pebbles deposit in front of the place where waves reach.
(4) Beach pebbles above 8mm tend to be flat, and those below 8mm tend to be sphered. That the shape of the larger pebbles becomes flat is probably ascribed to the fact that they only move occasionally, so that they are worn on their exposed surface by the wash of finer material. Spheroidal shape of the finer pebbles and granules are worn uniformly by rolling.
(5) The effects of abrasion on a beach shows stronger than in a river. Nevertheless, the decrease of grain size during drift is like in a river, owing rather to the sorting than to the abrasion.
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