Marine Science Faculty Publications
Document Type
Article
Publication Date
2005
Digital Object Identifier (DOI)
https://doi.org/10.1029/2005EO030002
Abstract
Fluvial sediment fills the coastal ocean, and sea level rise floods river valleys. This epic battle of terrestrial and marine processes occurs along all shorelines, and the complexities are especially well revealed in the Gulf of Papua, a foreland basin on the southern coast of New Guinea. Two hundred to four hundred million tons of sediment are supplied each year by the Fly and other rivers to a continental shelf that has been dissected by ancestors of these same rivers. The new sediment builds a large depositional feature known as a clinoform, which grows seaward and buries the record of earlier environments.
Rights Information
Was this content written or created while at USF?
Yes
Citation / Publisher Attribution
Eos, Transactions American Geophysical Union, v. 86, issue 3, p. 25-32
©2005. American Geophysical Union. All Rights Reserved.
Scholar Commons Citation
Crockett, J. S.; Nittrouer, C. A.; Ogston, A. S.; Sternberg, R. W.; Driscoll, N. W.; Babcock, J.; Milliman, J. D.; Slingerland, R.; Naar, D. F.; Donahue, B.; Walsh, J. P.; Dietrich, W.; Parker, G.; Bera, M.; Davies, H.; Harris, P.; Goni, M.; Aller, R.; and Aller, J., "Where Rivers and Oceans Collide" (2005). Marine Science Faculty Publications. 2211.
https://digitalcommons.usf.edu/msc_facpub/2211