Jump to content

Faroe-Bank Channel overflow

From Wikipedia, the free encyclopedia
This is an old revision of this page, as edited by DennVerm (talk | contribs) at 09:43, 10 March 2022 (Created page with '{{subst:AfC submission/draftnew}}<!-- Important, do not remove this line before article has been created. --> {{Draft article|Faroe-Bank Channel overflow|subject=natural sciences}} Through the Faroe-Bank Channel cold water from the Arctic Ocean is transported towards the northern parts of the Atlantic Ocean. This process is called '''Faroe-Bank Channel overflow'''. == References == <!-- Inline citations added to your article will automatical...'). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.
(diff) ← Previous revision | Latest revision (diff) | Newer revision → (diff)


Through the Faroe-Bank Channel cold water from the Arctic Ocean is transported towards the northern parts of the Atlantic Ocean. This process is called Faroe-Bank Channel overflow.




References