Abstract
The formative processes of Holocene strandplain ridges in the Kujukuri coastal plain have been frequently discussed. The ridges were indicated by land use which was shown on the old large-scale topographic maps called “Jinsoku-sokuzu”, the Rapid Survey Map during the middle of the Meiji period, around 1883. It is concluded that six groups of strandplain ridges developed in this coastal plain.