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The Denmark Strait overflow (Danish: Grønlandspumpen; Norwegian: Grønlandspumpa, meaning "the Greenland pump") is an undersea overflow located in the Denmark Strait between Greenland and Iceland. The overflow transports around 3.2 million m 3 (110 million cu ft) of water per second, greatly eclipsing the discharge of the Amazon River into the ...
The strait connects the Greenland Sea, an extension of the Arctic Ocean, to the Irminger Sea, a part of the Atlantic Ocean.It is 480 kilometres (300 mi) long. The narrowest part of the strait is 290 kilometres (180 mi) wide and lies between Straumnes, on Iceland's Hornstrandir peninsula, and Cape Tupinier, on Greenland's Blosseville Coast.
The Irminger Sea is a marginal sea of the North Atlantic Ocean.It is bordered to the west by southern Greenland, to the north by Iceland and the Denmark Strait, to the east by the Reykjanes Ridge (a northern part of the Mid-Atlantic Ridge), and to the south by open waters of the North Atlantic.
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The following are lists of waterfalls in the world by height, classified into two categories — natural and artificial. Natural waterfalls are further subdivided between overall height and tallest single drop. Each column (Waterfall, Height, Locality, Country) is sortable by using the up/down link in the column headings at the top of each column.
Water from the Fram Strait recirculates, reaching a density of DSOW, sinks, and flows towards the Denmark Strait. Water flowing into the Barents Sea feeds ISOW. ISOW enters the eastern North Atlantic over the Iceland-Scotland Ridge through the Faeroe Bank Channel at a depth of 850 m, with some water flowing over the shallower Iceland-Faeroe Rise.
Where an island is situated between a "belt" and a "sound", typically the broader strait is called "belt" and the narrower one is the "sound": Als: separated from the continent by Alssund; separated from Fyn by the southern part of the Little Belt, an area referred to in German (but not Danish) as Alsenbelt; Fehmarn
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