“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).
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).
- 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:10.1029/2004JE002309Google Scholar
- Holm DA (1957) Sigmoidal dunes – a transitional form. (abs). Geol. Soc. America Bull 68(12) 2, 1746Google Scholar
- Jackson JA (ed) (1997) Glossary of Geology, 4th edn. Am. Geol. Inst, Alexandria, p 769Google Scholar
- 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 1–19Google Scholar
- 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 403Google Scholar