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- W2081961330 abstract "Subaerial exposure beside the Wandandian Creek channel during the last glacial maximum led to the development of red and orange mottling and, in some areas, produced a palaeosol over the Pleistocene land surface. Incision of the palaeo-Wandandian Creek, during the Late Pleistocene, formed a relatively deep steep-sided channel partially infilled with medium-grained fluvial sand. This palaeovalley became drowned as the post-glacial marine transgression impounded the western portion of St Georges Basin and the basal prodelta/lagoonal mud facies was deposited from ca 7 ka. The Wandandian Creek delta prograded down the palaeovalley and reached the study area ∼3500 – 4000 years ago with the deposition of delta-front sandy silt and the overlying prograded sand facies. The subaerial portion of the delta is characterised by well-developed floodplains, levees, mouth bars and backswamps. Dredging in Wandandian Creek and land clearing for rural and urban development have had little long-term effect on the growth and morphology of Wandandian Creek delta." @default.
- W2081961330 created "2016-06-24" @default.
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- W2081961330 date "2006-12-01" @default.
- W2081961330 modified "2023-09-27" @default.
- W2081961330 title "Holocene stratigraphic and morphological evolution of the Wandandian Creek delta, St Georges Basin, New South Wales" @default.
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- W2081961330 doi "https://doi.org/10.1080/08120090600880909" @default.
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