Definition
“A dune that tends to develop unusual height but migrates only a limited distance because seasonal shifts in direction of the dominant wind cause it to move alternately in nearly opposite directions” (Jackson 1997, p. 545).
Description
Reversing dunes are intermediate in character between star and transverse dunes. They are similar to transverse dunes but have a secondary slip face which develops periodically and is oriented in an opposite direction from that of the primary slip face (McKee 1979).
Subtype
Sigmoidal dune. S-shaped or straight, triangular (Tsoar 2001), steep-sided, sharp-crested dune which is formed in response to alternating and opposing winds of roughly equal velocities (Holm 1957; Stone 1967; Edgell 2006) (Fig. 1).
Reversing slip faces containing bright material on double-sided (sigmoidal) barchan dunes in Proctor Crater, Mars. (a) MOC NA M1900307 during the fall (Ls = 45°) and (b) MOC NA E0902707 during the spring (Ls = 263°) show...
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References
Edgell HS (2006) Arabian deserts: nature, origin and evolution. Springer, Dordrecht
Fenton LK (2005) Potential sand sources for the dune fields in Noachis Terra, Mars. J Geophys Res 110:E11004. doi:10.1029/2005JE002436
Fenton LK, Bandfield JL, Ward AW (2003) Aeolian processes in Proctor Crater on Mars: sedimentary history as analyzed from multiple data sets. J Geophys Res 108(E12):5129. doi:10.1029/2002JE002015
Fenton LK, Toigo AD, Richardson MI (2005) Aeolian processes in Proctor Crater on Mars: mesoscale modeling of dune-forming winds. J Geophys Res 110:E06005. doi:10.1029/2004JE002309
Holm DA (1957) Sigmoidal dunes – a transitional form. (abs). Geol. Soc. America Bull 68(12) 2, 1746
Jackson JA (ed) (1997) Glossary of Geology, 4th edn. Am. Geol. Inst, Alexandria, p 769
McKee ED (1979) Introduction to a study of global sand seas. In: McKee ED (ed) A study of global sand seas. U.S. geological survey professional paper, U.S. Govt. Print. Off., Washington vol 1052. pp 1–19
Silvestro S, Di Achille G, Ori GG (2010) Dune morphology, sand transport pathways and possible source areas in east Thaumasia Region (Mars). Geomorphology 121:84–97. doi:10.1016/j.geomorph.2009.07.019
Silvestro S, Fenton LK, Michaels TI, Valdez A, Ori GG (2012) Interpretation of the complex dune morphology on Mars: dune activity, modelling and a terrestrial analogue. Earth Surf Proc Land 37(13):1424–1436. doi:10.1002/esp.3286
Stone RO (1967) A desert glossary. Earth Sci Rev 3:211–268
Tsoar H (2001) Types of Aeolian sand dunes and their formation. In: Balmforth NJ, Provenzale A (eds) Geomorphological fluid mechanics, Lecture notes in physics 582. Springer, p 403
Zimbelman JR (2010) Transverse Aeolian Ridges on Mars: first results from HiRISE images. Geomorphology 121:22–29. doi:10.1016/j.geomorph.2009.05.012
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Silvestro, S., Hermas, E. (2015). Reversing Dune. In: Hargitai, H., Kereszturi, Á. (eds) Encyclopedia of Planetary Landforms. Springer, New York, NY. https://doi.org/10.1007/978-1-4614-3134-3_305
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DOI: https://doi.org/10.1007/978-1-4614-3134-3_305
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