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• W4386957629 startingPage "277" @default.
• W4386957629 abstract "The deposits of Sydney’s rivers are thought to have experienced widespread aeolian modification during the Quaternary. The resultant sediments form archaeologically important landscapes upon which are found several of the oldest archaeological sites in the Sydney district. Unfortunately, little is known of the processes and products of aeolian reworking. The context of the archaeological discoveries is therefore enigmatic. This study focusses on the Agnes Banks Sand, a Cenozoic sand body that may represent the only sedimentary unit in the Sydney area that preserves reliable evidence of the action of aeolian processes on fluvial sediments. Our work confirms that the sands are indistinguishable from inland dune deposits worldwide, with the deposits reworked from alluvial sediments within and adjacent to the channel of the nearby Nepean River. The sands form east–west-aligned linear dunes, whilst the sediment body fines to the east, a pattern consistent with entrainment by westerly winds." @default.
• W4386957629 created "2023-09-23" @default.
• W4386957629 creator A5008595951 @default.
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• W4386957629 date "2023-07-03" @default.
• W4386957629 modified "2023-10-11" @default.
• W4386957629 title "Wind-reworked fluvial deposits as an archaeological environment: the Agnes Banks Sand of the Quaternary Hawkesbury–Nepean sequence of southeast Australia" @default.
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• W4386957629 doi "https://doi.org/10.1080/00049182.2023.2250157" @default.
• W4386957629 hasPublicationYear "2023" @default.
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