| 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 |
| Genre: | Article |
| ProdID: | 70016473 |
| Citation Author: | Rubin, D. M. |
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| Citation End Page: | 14 |
| Citation Issue: | 1 |
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| Citation Language: | English |
| Citation Larger Work Title: | Earth Surface Processes and Landforms |
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| Citation Number Of Pages: | 14 |
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| Citation Publisher: | Wiley |
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| Citation Search Results Text: | Lateral migration of linear dunes in the Strzelecki Desert, Australia; 1990; Article; Journal; Earth Surface Processes and Landforms; Rubin, D. M. |
| Citation Start Page: | 1 |
| Citation Volume: | 15 |
| Citation Year: | 1990 |
| Type: | citation/reference |
| Text: | Lateral migration of linear dunes in the Strzelecki Desert, Australia; 1990; Article; Journal; Earth Surface Processes and Landforms; Rubin, D. M. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| URL (DIGITAL OBJECT IDENTIFIER): | http://dx.doi.org/10.1002/esp.3290150102 |
| Date Other: | Mon, 1 Jan 1990 00:00 -0600 |
| Publisher: | Wiley |
