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This paper intends to clarify why and how such a huge tombolo having a surface area of 1,700,000 m2 has been formed at the west coast of Iwojima for relatively short period of 33 years after 1945. Analyses are performed on various data obtained through literature survey and field measurements to determine the growth rate of tombolo and variation rate of shore and sea floor surrounding the island. Model tests are also made on the formation of tombolo. The followings are the conclusions deriveddoi:10.9753/icce.v19.96 fatcat:4ugnf7ezxvaq7g5ggnnxow2rmu