- Abstract:
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Sand ramps occur on a continuum of topographically-controlled landforms, ranging from purely aeolian features (climbing/falling dunes) to talus cones and alluvial fans. Sand ramps have been identified as potentially important palaeoenvironmental archives in dryland regions that possess relatively few Quaternary proxy records. Their utility however requires not only good age control of depositional phases but clear identification of process regimes, determined through morphological and sedimen...
Expand abstract - Publication status:
- Published
- Peer review status:
- Peer reviewed
- Version:
- Accepted Manuscript
- Files:
-
-
(pdf, 1.5mb)
-
- Publisher copy:
- 10.1016/j.geomorph.2018.03.021
-
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- Publisher:
- Elsevier Publisher's website
- Journal:
- Geomorphology Journal website
- Volume:
- 311
- Pages:
- 103-113
- Publication date:
- 2018-03-29
- Acceptance date:
- 2018-03-23
- DOI:
- EISSN:
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1872-695X
- ISSN:
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0169-555X
- Pubs id:
-
pubs:831987
- URN:
-
uri:9ce83349-3251-4b0b-818e-ce5a39f852a4
- UUID:
-
uuid:9ce83349-3251-4b0b-818e-ce5a39f852a4
- Local pid:
- pubs:831987
- Keywords:
- Copyright holder:
- Elsevier B.V.
- Copyright date:
- 2018
- Notes:
-
Copyright © 2018 Elsevier B.V. This is the accepted manuscript version of the article. The final version is available online from Elsevier at: https://doi.org/10.1016/j.geomorph.2018.03.021
Journal article
Sand ramps as palaeoenvironmental archives: Integrating general principles and regional contexts through reanalysis of the Klipkraal Sands, South Africa
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