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Ikertooq Fjord

fjord in Greenland

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Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionMar 25, 2025
Entity authorityQ5995890 ↗
Source-derived summary

Ikertooq Fjord (old spelling: Ikertôq) is a 55 km (34 mi) long fjord in the Qeqqata municipality in western Greenland. The fjord empties into Davis Strait 21 km (13 mi) south of Sisimiut.

Geography

The upper part of the fjord, a confluence of three tributary inlets at approximately 66°53′20″N 52°32′00″W is called Suluppaavarsiorfik (old spelling: Sulugpâvarsiorfik). The tributary bays, from south to north, are: Avalleq, Akulleq (the innermost, main arm at approximately 66°55′50″N 52°16′00″W), and Maligiaq. Itinneq, an outflow river from the large, latitudinal Tasersuaq lake, empties into the northern inlet.

The fjord initially flows westward, to then turn west-south-west between the mainland peninsula in the south, and Sarfannguit Island in the north, widening considerably at its mouth at approximately 66°46′N 53°27′W, where it empties into Davis Strait. The fjord is unusual in that it connects through a very narrow waterway to the head of the narrower Amerloq Fjord near the village of Sarfannguit.

The northern inlet at the fjord head is surrounded by tall mountains immediately to the south of the Pingu mountain group halfway between Davis Strait and the Greenland ice sheet (Greenlandic: Sermersuaq). The range flattens considerably towards the east in the area of Kangaamiut dike swarm north of Kangerlussuaq, due to pressure exerted by the icesheet for long periods in the past.

Settlement

The small Sarfannguit settlement occupies the eastern promontory on Sarfannguit Island, on the northern shore of the fjord, at the narrow waterway between the mainland and Sarfannguit Island.

Editorial summary

This brief starts where responsible research should: with the source description of “Ikertooq Fjord” as fjord in Greenland. Everything that follows is an evidence route, not borrowed authority.

Editorial reviewA practical starting point whose main value is the path it opens into stronger specialist and primary sources. The current 245-word lead offers orientation but no explicit four-digit date, so chronology should not be assumed. The selected authority fields contribute no independent date. The account is most persuasive where Ikertooq, Fjord and fjord can be independently traced.
Editorial analysis

Why this record matters

The subject matters to the general reference register because the source frames it as fjord in Greenland. Its deeper value depends on whether names, dates, institutions and citations support that framing.

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 Mar 25, 2025. The linked authority identifier is Q5995890. Authority coordinates are 66.867, -52.833. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank.

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 “Ikertooq Fjord” 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.