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Understanding continent-ocean sediment transfer

Authors :
Mulder, Thierry
Cirac, Pierre
Gaudin, Mathieu
Bourillet, Jean-francois
Trainer, J.
Normand, Alain
Weber, O.
Griboulard, R.
Jouanneau, Jean-marie
Anschutz, Pierre
Jorissen, Frans
Mulder, Thierry
Cirac, Pierre
Gaudin, Mathieu
Bourillet, Jean-francois
Trainer, J.
Normand, Alain
Weber, O.
Griboulard, R.
Jouanneau, Jean-marie
Anschutz, Pierre
Jorissen, Frans
Source :
EOS, Transactions American Geophysical Union (0096-3941) (AGU), 2004-07-06 , Vol. 85 , N. 27 , P. 257
Publication Year :
2004

Abstract

Submarine canyons are narrow but deep submarine valleys that extend for hundreds of meters. They represent the most impressive structures that shape the present morphology of passive continental margins. They can occur off the mouth of rivers: the Tagus, Zaire, Amazon, and Orinoco in the Atlantic; the Indus in the Indian Ocean; and the Var, Rhone, and Ebro in the Mediterranean. Some are at times disconnected from any stream mouth such as the Nazare canyon, off Portugal, despite the fact that it is close to the coast. Some were connected to a river mouth during lowstands of sea level, such as the Wilmington canyon in the northwest Atlantic, or the Blackmud canyon in the northeast Atlantic.

Details

Database :
OAIster
Journal :
EOS, Transactions American Geophysical Union (0096-3941) (AGU), 2004-07-06 , Vol. 85 , N. 27 , P. 257
Notes :
application/pdf, English
Publication Type :
Electronic Resource
Accession number :
edsoai.on1286189530
Document Type :
Electronic Resource
Full Text :
https://doi.org/10.1029.2004EO270001