Abstract
Any riparian forest stands on landforms which are formed, maintained and altered by fluvial processes. Activity of fluvial processes is therefore the matter of principal concern in the study of riparian vegetation. Fluvial processes in the broad sense (Leopold et al. 1964) include both stream action, that is fluvial processes in the narrow sense, and mass-movements, that is customarily classified as hillslope processes (Carson & Kirkby 1972). Although relatively frequent events of flood provide fluvial sediments, mass-movements which occur less frequently bring about alteration of landforms and substrata of not only valley sides but also valley bottoms in upstream watersheds.
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Tamura, T. (2008). Occurrence of hillslope processes affecting riparian vegetation in upstream watersheds of Japan. In: Sakio, H., Tamura, T. (eds) Ecology of Riparian Forests in Japan. Springer, Tokyo. https://doi.org/10.1007/978-4-431-76737-4_2
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DOI: https://doi.org/10.1007/978-4-431-76737-4_2
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