Abstract
Maury Channel is a 3,500-km-long, erosional/depositional feature. Originating on the southern slope of the Faeroe-Iceland Ridge at about 64° N., 13° W., the channel follows the deepest axis of Rockall Basin until about 53° N., where it begins a meandering course through several northeast Atlantic fracture zones. The channel finally empties into the northern Iberian Basin. Turbidity currents and overflow boulses of Norwegian Sea deep water are thought to be responsible for the formation of the channel. Strong bottom currents are responsible for keeping the channel “open” south of 53° N. Seismic reflection profiles reveal a characteristic “signature,” indicating deposition of dense turbidite material wherever the channel is encountered.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
