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Do pediplains exist? Suggested criteria and examples

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Pediplains are formed by the coalescence of pediments and by implication are of considerable areal extent. But the nature of the component pediments and the size of the area covered have not been specified. Three types of pediments of similar morphology but of different structure, distribution and perceived origins, have been described. Mantled pediments of etch origin are the most widely distributed and examples now lacking a backing scarp are recognized. Selected Australian regions are considered as possible as examples of pediplains. Areas of regional extent with prominent mantled pediments but also significant areas of upland and alluviated plains are differentiated from pedimented landscapes in which scarpless mantled forms are dominant. Many suggested pediplains are also inselberg landscapes.
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Document Type: Research Article

Publication date: December 1, 2013

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  • Zeitschrift für Geomorphologie main volume is a peer-reviewed international journal presenting original contributions of high scientific standard from all fields of geomorphology, encompassing basic research and applied studies. Zeitschrift für Geomorphologie (ZfG) invites the submission of original papers from the entire field of geomorphological research, both applied and theoretical. Authors are encouraged to submit their papers to the editor-in-chief. Please peruse the instructions to authors (PDF) before submitting your paper.

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