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Cape York meteorite

very large iron meteorite from Greenland

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General referenceInterpretive dossier study · Crown Archives visual atlas
Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionJul 1, 2026
Entity authorityQ1034516
Source-derived summary

The Cape York meteorite, also known as the Innaanganeq meteorite, is one of the largest known iron meteorites, classified as a medium octahedrite in chemical group IIIAB. In addition to many small fragments, at least eight large fragments with a total mass of 58 tonnes (128,000 lb) have been recovered, the largest weighing 31 tonnes (68,000 lb). The meteorite was named after Cape York, a prominent geographic feature located approximately 48 kilometres (30 mi) west of the east coast of Meteorite Island and the nearby peninsulas in northern Melville Bay, Greenland, where the first meteorite fragments were discovered.

The date of the meteorite fall is debated, but was likely within the last few thousand years. A museum placard accompanying the Agpalilik fragment at the Natural History Museum of Denmark states it fell approximately 58 million years ago. This figure is inconsistent with the archaeological/historical estimate that the fall occurred within the last 1,000–10,000 years, and does not match published terrestrial-age estimates of 1–2 million years. The 58-million-year figure is roughly the same order of magnitude as Cape York's cosmic-ray exposure age of 93 ± 16 million years, suggesting the signage may conflate time spent in space as a meteoroid with time spent on Earth since the fall.

It was known to the Inughuit (the local Inuit) for centuries, who used it as a source of meteoritic iron for tools.

History

Presumably the meteorite fell to Earth a few thousand years ago. Some estimates have put the date of the fall as 10,000 years ago.

All fragments recovered were found at the surface, partly buried, some on unstable terrain.

Editorial summary

This brief starts where responsible research should: with the source description of “Cape York meteorite” as very large iron meteorite from 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 268-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 Cape, York and meteorite can be independently traced.
Editorial analysis

Why this record matters

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

Evidence profile

Named sources, stable identifiers and responsible institutions provide the strongest route from overview to verifiable evidence. The source revision retrieved here is dated Jul 1, 2026. The linked authority identifier is Q1034516. Authority coordinates are 76.133, -64.933. 1 of 1 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank.

Critical limits

The absence of detail may reflect summary conventions rather than a lack of surviving documentation. 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.

How to read it

Use the entry as an orientation point, then follow its citations and revision history. Names, dates and institutional relationships should be checked against the original record.

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Source & attribution

This entry incorporates text from Cape York meteorite” 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.