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Moskstraumen

tidal whirlpool system at the Lofoten archipelago in Norway

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Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionSep 14, 2026
Entity authorityQ1501474
Source-derived summary

Moskstraumen or Moskenstraumen, also known as the Lofoten maelstrom, is a system of tidal eddies and whirlpools, one of the strongest in the world, that forms at the Lofoten archipelago in Nordland county, Norway between the Norwegian Sea and the Vestfjorden. It is located between the Lofoten Point (Norwegian: Lofotodden) on the island of Moskenesøya (in Moskenes Municipality) and the island of Mosken (in Værøy Municipality). Moskstraumen is unusual in that it occurs in the open sea, whereas most other tidal flows are observed in confined straits or rivers. It originates from a combination of several factors, the dominant being the strong semi-diurnal tides and peculiar shape of the seabed, with a shallow ridge between the Moskenesøya and Værøya islands which amplifies and whirls the tidal currents.

Moskstraumen has been featured in many historical accounts, generally exaggerated. It is also popularly known as maelstrom – a Nordic word (malstrøm/malström) for a strong whirlpool which originates from the Dutch combination of malen (to grind) and stroom (stream). This term was introduced into the English language by Edgar Allan Poe in 1841, through his short story "A Descent into the Maelström". Poe provides an alternative name for the whirlpool with the line: "We Norwegians call it the Moskoestrom, from the island of Moskoe in the midway."

Description and mechanism

Moskstraumen is located between the Lofoten Point of the island of Moskenesøya (in Moskenes Municipality) and the small island of Mosken in Værøy Municipality. It involves strong tidal currents flowing through the shallows between these islands and the Atlantic Ocean and the deep Vestfjorden, creating large, weak eddies and small whirlpools. In 1986, the Norwegian Hydrographic Service published a pilot book saying that currents could reach strengths of 5 metres per second, although a 1997 study found a maximum strength of 3 m/s and ship-based measurements in 1999 measured currents of 1.7 m/s.

Editorial summary

Begin with the source’s own compact description: “Moskstraumen” is tidal whirlpool system at the Lofoten archipelago in Norway. The dossier treats that line as a proposition to test through Moskstraumen, tidal and whirlpool, not as a finished interpretation.

Editorial reviewA dependable orientation record for establishing vocabulary, names and a first evidence trail. The current lead gives the account dated anchors—1841, 1986, 1997, 1999—that can be checked directly. The selected authority fields contribute no independent date. For this dossier, Moskstraumen, tidal and whirlpool is the immediate research focus.
Editorial analysis

Why this record matters

The phrase “tidal whirlpool system at the Lofoten archipelago in Norway” supplies a clear boundary for inquiry. It also exposes the unanswered questions: who defined that boundary, when it became stable and which sources sit outside it.

Evidence profile

The citation trail is more important than the brevity of the summary: it shows where individual claims can be examined in context. The source revision retrieved here is dated Sep 14, 2026. The linked authority identifier is Q1501474. VIAF identifies the subject as 239663758. Authority coordinates are 67.800, 12.833. 1 of 2 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank. The first chronological checks are 1841, 1986, 1997 and 1999.

Critical limits

Overview language is designed for orientation and should not be treated as a substitute for the evidence cited beneath it. The source lead contains qualifying language; that uncertainty should survive quotation, summary and reuse. Authority statements aid reconciliation but still require their own references, qualifiers and ranks to be checked.

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Source & attribution

This entry incorporates text from Moskstraumen” on English Wikipedia. Contributors are listed in the page history. Text is available under the Creative Commons Attribution-ShareAlike 4.0 License. Selected authority identifiers and statements are retrieved from Wikidata under CC0; their references and qualifiers remain part of the verification path.