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Geomorphology of Desert Environments pp 265–299Cite as

Badlands and Gullying

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Badlands have fascinated geomorphologists for the same reasons that they inhibit agricultural use: lack of vegetation, steep slopes, high drainage density, shallow to non-existent regolith, and rapid erosion rates. Badlands appear to offer in a miniature spatial scale and a shortened temporal scale many of the processes and landforms exhibited by more normal fluvial landscapes, including a variety of slope forms, bedrock or alluvium-floored rills and washes, and flat alluvial expanses similar to large-scale pediments. Although badlands evoke an arid image, they can develop in nearly any climate in soft sediments where vegetation is absent or disturbed.

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  1. Department of Environmental Sciences, University of Virginia, Charlottesville, VA 22904-4123, USA

    Alan D. Howard

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  1. Dept. Geography, University of Sheffield, Winter Street, Sheffield, United Kingdom S10 2TN

    Anthony J. Parsons

  2. Dept. Geography, State University of New York, Buffalo, NY 14261, USA

    Athol D. Abrahams

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Howard, A.D. (2009). Badlands and Gullying. In: Parsons, A.J., Abrahams, A.D. (eds) Geomorphology of Desert Environments. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-5719-9_10

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