Norwegian Sea overflow through the Faroe-Shetland gateway as documented by its bedforms

We have used seabed information from three deep-tow side-scan sonar surveys in order to trace the high-energy current core of Norwegian Sea Overflow Water (NSOW) from the Faroe–Shetland Channel (FSC) through the Faroe Bank Channel (FBC) towards the southern flank of the Iceland–Faroe Ridge. A hierar...

Full description

Bibliographic Details
Published in:Marine Geology
Main Authors: Kuijpers, A., Hansen, B., Huehnerbach, V., Larsen, B., Nielsen, T., Werner, F.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2002
Subjects:
Online Access:https://eprints.soton.ac.uk/43909/