The positions of the Chinda (Odaki) Falls have been recorded in historical documents and paintings since the late 15th century. This study aimed to estimate the recession rates of the Chinda Falls by tracing the history of its retreat.
The earliest painting of the Chinda Falls by Sesshu in 1476 indicates that the Odaki Falls was located downstream within 333 m of its present position. A regional geography of Bungo province completed in 1803 mentioned that the Odaki Falls in 1799 was lowered 114-223 m from the current location. In 1909, a dam was constructed 60-70 m above the Odaki Falls for hydroelectric power generation. Subsequently, Odaki Falls continued its recession, approaching within 20 m of the dam in 1952, and has been controlled by artificial reinforcement since then to prevent damaging the dam by waterfall retreat. The present Odaki Falls is located 17.5 m downstream from the dam.
The average recession rate of the Odaki Falls was less than 0.7 m/year in the last 500 years. Additionally, the following variations in recession rates of the Odaki Falls were observed during this period. The calculated recession rate from 1476 to 1799 was less than 0.7 m/year, while that from 1799 to 1909 was 0.6-1.6 m/year, and that from 1909 to 1952 was 0.9-1.2 m/year. The results show that the recession rate of the Odaki Falls has varied three times at most during the last 500 years. The estimated recession rate after the deposition of Aso-4 welded ignimbrite (90 ka B.P.) was 0.36 m/year.
From the above, the recession rate of the Odaki Falls possibly increased during the 19th century. However, the number of recorded natural disasters represented by floods, earthquakes, and volcanic eruptions did not increase in the same period. These results indicate that the century-scale environmental changes around the Odaki Falls barely increased or decreased the recession rate of that waterfall.
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