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Bedrock-alluvial streams with knickpoint and plunge pool that migrate upstream with permanent form
Purely alluvial rivers cannot sustain knickpoints along their long profiles, as they would be obliterated by diffusional morphodynamics. Bedrock streams with a partial alluvial cover, however, form and sustain slope breaks over long periods of time. Here we consider the case of an initial profile of...
Autores principales: | , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2019
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6467923/ https://www.ncbi.nlm.nih.gov/pubmed/30992477 http://dx.doi.org/10.1038/s41598-019-42389-2 |