Geomorphic evidence of major sea-level fluctuations during marine isotope substage-5e, Cape Cuvier, Western Australia
A detailed geomorphologic and morphostratigraphic investigation of raised marine terraces at Cape Cuvier, Western Australia, reveals two morphologically distinct units. A lower, well-developed accretional reef terrace between 3 and 5.5 m above MLWS (mean low-water springs; hereafter denoted as “+”)...
| Main Authors: | , , |
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| Format: | Journal Article |
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Elsevier BV
2008
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| Online Access: | http://hdl.handle.net/20.500.11937/41970 |