Geomorphic reconstruction of formation and recession processes of waterfalls of the Kaminokawa river basin on Osumi Peninsula, southern Kyushu, Japan
Author:
Affiliation:
1. Department of Geography, Faculty of Arts and Letters; Meiji University; Tokyo Japan
2. Center for Spatial Information Science; University of Tokyo; Kashiwa Japan
Publisher
Wiley
Subject
Earth-Surface Processes,Geography, Planning and Development
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/1745-5871.12229/fullpdf
Reference67 articles.
1. Geologically controlled waterfall types in the Outer Carpathians;Alexandrowicz;Geomorphology,1994
2. Ata pyroclastic flows and the Ata caldera in Southern Kyushu, Japan;Aramaki;Journal of the Geological Society of Japan,1966
3. Knickpoint recession rate and catchment area: the case of uplifted rivers in eastern Scotland;Bishop;Earth Surface Processes and Landforms,2005
4. Knickpoint initiation and distribution within fluvial networks: 236 waterfalls in the Waipaoa River, North Island, New Zealand;Crosby;Geomorphology,2006
5. Retrogression rate of the Victoria Falls and the Batoka Gorge;Derricourt;Nature,1976
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1. Landform Development of Kimotsuki Plain before Deposition of Osumi Pumice Fall, Kyushu, Japan: Formation of Buried Ata Welded Ignimbrite Plateau beneath Ito Ignimbrite;Journal of Geography (Chigaku Zasshi);2022-06-25
2. Waterfalls: Forms, Distribution, Processes and Rates of Recession;Quaestiones Geographicae;2020-03-01
3. Recession Rates of Knickpoints at Different Timescales in the Ata Ignimbrite, Satsuma Peninsula, Southwest Japan;Geographical review of Japan series A;2019-05-01
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