Geomorphic reconstruction of formation and recession processes of waterfalls of the Kaminokawa river basin on Osumi Peninsula, southern Kyushu, Japan. (28th February 2017)

• Record Type: Journal Article
• Authors: Yoshida, Hidetsugu; Hayakawa, Yuichi S.; Takanami, Shintaro; Hikitsu, Akira; Ohsaka, Saki; Ishii, Ryo
• Is Part Of: Geographical research. Volume 55:Number 4(2017)
• Page Start: 424
• Page End: 437
• Publication Date: 2017-02-28
• Subjects: waterfall -- recession rate -- Ata pyroclastic flow -- ignimbrite -- knickpoint; Geography -- Research -- Periodicals; Geography -- Australasia -- Periodicals; Human geography -- Periodicals; Physical geography -- Periodicals; 304.2072
• DOI: 10.1111/1745-5871.12229
• Languages: English
• ISSNs: 1745-5863

Abstract

Abstract: To assess the geomorphological importance of waterfall recession in volcanic bedrock, we examined recession rates of six waterfalls in the lower reaches of Kaminokawa river basin on the Osumi Peninsula in southern Kyushu. The examination was performed with an empirical equation that uses a dimensionless parameter obtained by dimensional analysis of relevant measured factors, including erosive force, size of waterfall, and bedrock resistance. Welded Ata ignimbrite, formed at approximately 110 ka, may have played an initiating role to maintain such waterfalls because it resists weathering more than other local rocks. Estimated recession rates for the six waterfalls range from 0.2 to 3.0 cm/y, which compare with estimated rates for waterfalls in another region characterised by welded ignimbrite. Comparison of equation‐derived recession rates of waterfalls with actual recession distances from confluences supports the idea that an original waterfall will subsequently split into two distinct waterfalls when it recesses past an upstream junction of two channels. Our findings revealed that all six waterfalls likely would have been at almost the same point lower in the watershed in the past, marking the general site of the original waterfall. Moreover, the ancestral original waterfall is highly likely to have started from a point between the caldera rim and present river mouth. There, a knickpoint was likely caused by the river dropping into an inner part of the caldera, possibly just after the eruption of the Ata ignimbrite. The waterfall erodes upstream away from the caldera basin, and this happens to be to the east.