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Geomorphology of Desert Environments pp 413–467Cite as

Processes and Forms of Alluvial Fans

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Alluvial fans are a conspicuous conical landform commonly developed where a channel emerges from a mountainous catchment to an adjoining valley (Figs. 14.1 and 14.2). Although present in perhaps all global climates, fans in deserts have been the most studied due to their excellent exposure and ease of access. Drew (1873), working in the upper reaches of the Indus River valley in the western Himalaya of India, provided the earliest illustrations and scientific description of desert alluvial fans (pp. 445–447):

Keywords

  • Geological Society
  • Rock Avalanche
  • Fault Scarp
  • Mountain Front
  • Rock Slide

These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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    Athol D. Abrahams

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Blair, T.C., McPherson, J.G. (2009). Processes and Forms of Alluvial Fans. In: Parsons, A.J., Abrahams, A.D. (eds) Geomorphology of Desert Environments. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-5719-9_14

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