Lateral migration of linear dunes in the Strzelecki Desert, Australia
Earth Surface Processes and Landforms
By: D. M. Rubin
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Abstract
Preferential accumulation of sand on east-facing flanks indicates that the dunes migrated eastward several metres during the Holocene. Moreover, the west-facing flanks of some dunes have experienced a minimum of tens of metres of erosion. This asymmetric erosion and deposition were caused by dune obliquity and lateral migration that may have begun as early as the Pleistocene. Dunes in the Strzelecki Desert and in the adjacent Simpson Desert display a variety of grossly different internal structures. -from Author
Suggested Citation
Rubin, D.M., 1990, Lateral migration of linear dunes in the Strzelecki Desert, Australia: Earth Surface Processes and Landforms, v. 15, no. 1, p. 1-14, https://doi.org/10.1002/esp.3290150102.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Lateral migration of linear dunes in the Strzelecki Desert, Australia |
| Series title | Earth Surface Processes and Landforms |
| DOI | 10.1002/esp.3290150102 |
| Volume | 15 |
| Issue | 1 |
| Publication Date | September 26, 2006 |
| Year Published | 1990 |
| Language | English |
| Publisher | Wiley |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Earth Surface Processes and Landforms |
| First page | 1 |
| Last page | 14 |