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• W2045843947 abstract "The far north Queensland coast is characterised by a juxtaposition of coral reefs and terrigenous sediment bodies. Consequently, the distribution and long‐term fate of coastal coral reefs is largely controlled by the processes responsible for sediment dispersal and accumulation. The marine environments which bound the northern Cape York Peninsula receive relatively little modern terrigenous sediment. Estimates of total riverine sediment reaching the coast north of latitude 12°S are 1 Mt y‐1 for the Great Barrier Reef coast and 2.4 Mt y‐2 for the Gulf of Carpentaria coast, corresponding to sediment fluxes (on the shore‐attached wedges) of 2000 g m2y‐1 and 800 g m2y‐1 respectively, and net rates of vertical sediment accumulation of terrigenous material of 0.4 mm y‐1 and 1 mm y‐1. The dispersal of terrigenous sediment appears to be controlled largely by coastline orientation with respect to onshore winds. On the Great Barrier Reef coast, sediment is transported northwards within a well‐defined inner‐shelf zo..." @default.
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• W2045843947 date "1998-08-01" @default.
• W2045843947 modified "2023-09-27" @default.
• W2045843947 title "Controls upon inner‐shelf sedimentation, Cape York Peninsula, in the region of 12°S" @default.
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• W2045843947 doi "https://doi.org/10.1080/08120099808728416" @default.
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