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Landscapes of Japan, 11, Beach at Noda.

Beach at Noda

Beach at Noda. -- Where there are indentations or bays along coastlines, wave action is reduced. In these more sheltered environments sediment which has been carried along the coast or brought to the bay by rivers from the land, may accumulate forming bars and beaches. If such deposition continues for a period of time, the bay may gradually fill, producing a level plain in the former coastal indentation. There are many such coastal plains along the Japanese shoreline, most of them small and isolated. -- Here, at Noda, barriers have been placed just offshore to further reduce wave action and promote deposition and beach formation and retention.
 
Editorial assistant: Joseph Augustin. Collection librarian: Amy Bryant. Please send any questions, comments, or content corrections to Michael Thiedeman, Professor of Art, Earlham College, Richmond, IN 47374 USA. email address: thiedmi@earlham.edu -- For specific reference to the images in the Landscapes of Japan set, you are invited to contacted Dr. Charles Martin, Professor Emeritus, Dept. of Geology, Earlham College, email address: martich@earlham.edu