Source: wikibot/faroe-bank-channel-overflow
= Faroe-Bank Channel overflow
{wiki=Faroe-Bank_Channel_overflow}
The Faroe-Bank Channel overflow refers to a significant oceanographic phenomenon occurring in the North Atlantic Ocean, specifically involving the movement of dense water from the Nordic Seas into the Atlantic. The Faroe-Bank Channel is a deep underwater trench located between the Faroe Islands and the Scottish coast.