The very slow chemical and physical weathering rates in desert areas coupled with a relatively high efficiency of wash processes, due to the general sparseness of vegetation, results in more widespread occurrence of slopes with little or no regolith than in areas with humid climates. This chapter outlines the processes and landforms occurring on desert slopes that are either massive bedrock or are scarps and cuestas in layered rocks dominated by outcropping resistant rock layers.

Keywords

Clay Calcite Cretaceous Leaching Gravel 

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Copyright information

© Springer Science+Business Media B.V. 2009

Authors and Affiliations

  • Alan D. Howard
    • 1
  • Michael J. Selby
    • 2
  1. 1.Department of Environmental SciencesUniversity of VirginiaCharlottesvilleUSA
  2. 2.Department of Earth SciencesUniversity of WaikatoHamiltonNew Zealand

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