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Badland landscape response to individual geomorphic events

Landscapes form by the erosion and deposition of sediment, driven by tectonic and climatic forcing. The principal geomorphic processes of badland – landsliding, debris flow and runoff erosion – are similar to those in full scale mountain topography, but operate faster. Here, we show that in the badl...

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Detalles Bibliográficos
Autores principales:	Yang, Ci-Jian, Turowski, Jens M., Hovius, Niels, Lin, Jiun-Chuan, Chang, Kuo-Jen
Formato:	Online Artículo Texto
Lenguaje:	English
Publicado:	Nature Publishing Group UK 2021
Materias:	Article
Acceso en línea:	https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8324919/ https://www.ncbi.nlm.nih.gov/pubmed/34330899 http://dx.doi.org/10.1038/s41467-021-24903-1

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