Matches in SemOpenAlex for { <https://semopenalex.org/work/W2592685098> ?p ?o ?g. }
- W2592685098 endingPage "437" @default.
- W2592685098 startingPage "424" @default.
- W2592685098 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." @default.
- W2592685098 created "2017-03-16" @default.
- W2592685098 creator A5024698741 @default.
- W2592685098 creator A5034449252 @default.
- W2592685098 creator A5047252276 @default.
- W2592685098 creator A5053020683 @default.
- W2592685098 creator A5062382815 @default.
- W2592685098 creator A5088823009 @default.
- W2592685098 date "2017-02-28" @default.
- W2592685098 modified "2023-10-01" @default.
- W2592685098 title "Geomorphic reconstruction of formation and recession processes of waterfalls of the Kaminokawa river basin on Osumi Peninsula, southern Kyushu, Japan" @default.
- W2592685098 cites W1533315712 @default.
- W2592685098 cites W1582979715 @default.
- W2592685098 cites W1986082054 @default.
- W2592685098 cites W1991123376 @default.
- W2592685098 cites W1993999355 @default.
- W2592685098 cites W1995521250 @default.
- W2592685098 cites W2001596430 @default.
- W2592685098 cites W2004227742 @default.
- W2592685098 cites W2006259982 @default.
- W2592685098 cites W2009711555 @default.
- W2592685098 cites W2020364089 @default.
- W2592685098 cites W2022119185 @default.
- W2592685098 cites W2025248405 @default.
- W2592685098 cites W2025278340 @default.
- W2592685098 cites W2043348511 @default.
- W2592685098 cites W2052074187 @default.
- W2592685098 cites W2053742084 @default.
- W2592685098 cites W2057345174 @default.
- W2592685098 cites W2059383495 @default.
- W2592685098 cites W2062583264 @default.
- W2592685098 cites W2066166725 @default.
- W2592685098 cites W2067994160 @default.
- W2592685098 cites W2069546454 @default.
- W2592685098 cites W2071237400 @default.
- W2592685098 cites W2076062906 @default.
- W2592685098 cites W2077047040 @default.
- W2592685098 cites W2080528192 @default.
- W2592685098 cites W2082950600 @default.
- W2592685098 cites W2087747927 @default.
- W2592685098 cites W2088051823 @default.
- W2592685098 cites W2088349978 @default.
- W2592685098 cites W2099770849 @default.
- W2592685098 cites W2127030045 @default.
- W2592685098 cites W2127886814 @default.
- W2592685098 cites W2131125610 @default.
- W2592685098 cites W2141892686 @default.
- W2592685098 cites W2150354081 @default.
- W2592685098 cites W2151322278 @default.
- W2592685098 cites W2162495231 @default.
- W2592685098 cites W2325730115 @default.
- W2592685098 cites W2328460140 @default.
- W2592685098 cites W2330161929 @default.
- W2592685098 cites W2334947589 @default.
- W2592685098 cites W938574615 @default.
- W2592685098 doi "https://doi.org/10.1111/1745-5871.12229" @default.
- W2592685098 hasPublicationYear "2017" @default.
- W2592685098 type Work @default.
- W2592685098 sameAs 2592685098 @default.
- W2592685098 citedByCount "3" @default.
- W2592685098 countsByYear W25926850982019 @default.
- W2592685098 countsByYear W25926850982020 @default.
- W2592685098 countsByYear W25926850982022 @default.
- W2592685098 crossrefType "journal-article" @default.
- W2592685098 hasAuthorship W2592685098A5024698741 @default.
- W2592685098 hasAuthorship W2592685098A5034449252 @default.
- W2592685098 hasAuthorship W2592685098A5047252276 @default.
- W2592685098 hasAuthorship W2592685098A5053020683 @default.
- W2592685098 hasAuthorship W2592685098A5062382815 @default.
- W2592685098 hasAuthorship W2592685098A5088823009 @default.
- W2592685098 hasConcept C109007969 @default.
- W2592685098 hasConcept C114793014 @default.
- W2592685098 hasConcept C120806208 @default.
- W2592685098 hasConcept C121012721 @default.
- W2592685098 hasConcept C123588078 @default.
- W2592685098 hasConcept C126645576 @default.
- W2592685098 hasConcept C127313418 @default.
- W2592685098 hasConcept C137527640 @default.
- W2592685098 hasConcept C165205528 @default.
- W2592685098 hasConcept C166957645 @default.
- W2592685098 hasConcept C17409809 @default.
- W2592685098 hasConcept C187320778 @default.
- W2592685098 hasConcept C205649164 @default.
- W2592685098 hasConcept C2778644228 @default.
- W2592685098 hasConcept C2780191791 @default.
- W2592685098 hasConcept C49708893 @default.
- W2592685098 hasConcept C58640448 @default.
- W2592685098 hasConcept C76886044 @default.
- W2592685098 hasConceptScore W2592685098C109007969 @default.
- W2592685098 hasConceptScore W2592685098C114793014 @default.
- W2592685098 hasConceptScore W2592685098C120806208 @default.
- W2592685098 hasConceptScore W2592685098C121012721 @default.
- W2592685098 hasConceptScore W2592685098C123588078 @default.
- W2592685098 hasConceptScore W2592685098C126645576 @default.
- W2592685098 hasConceptScore W2592685098C127313418 @default.
- W2592685098 hasConceptScore W2592685098C137527640 @default.
- W2592685098 hasConceptScore W2592685098C165205528 @default.
- W2592685098 hasConceptScore W2592685098C166957645 @default.