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Cape York meteorite

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Cape York meteorite
NameCape York
TypeIron
ClassMedium octahedrite
GroupIIIAB
Composition92% Fe, 7.6% Ni, 0.4% Co, 0.05% P, 2.4 ppm Ga, 0.13 ppm Ge, 0.8 ppm Ir
CountryGreenland
RegionAvannaata
Coordinates76, 08, N, 64...
Found dateKnown to the Inuit for centuries; recovered 1818–1984
Tkw58.2 t

Cape York meteorite. It is one of the largest iron meteorite masses known to have impacted Earth, with a total known weight exceeding 58 metric tons. The meteorite's fragments were known to the local Inuit peoples for centuries as a source of meteoric iron for tools and harpoon points before their scientific documentation by European explorers. Its recovery involved several major expeditions over more than a century, with the most famous pieces now housed in major museums, including the American Museum of Natural History and the Geological Museum of Copenhagen.

Discovery and recovery

The iron masses were known to the Inuit of northwestern Greenland long before European contact, referred to as "Savik" in their language, which means "iron" or "knife." The first recorded European discovery was made in 1818 by the British Arctic explorer John Ross, who learned of the "iron mountains" from local guides near Melville Bay. The first significant recovery was made in 1894 by the American explorer Robert Peary, who, with assistance from his assistant Matthew Henson and local Inuit, located and transported three massive fragments—Ahnighito, The Woman, and The Dog—from Savissivik to the coast using a specially built railroad. These were shipped to the United States and sold to the American Museum of Natural History. Further significant fragments, including Agpalilik (the "Man") weighing about 20 tons, were located and recovered by the Danish explorer Vagn Buchwald in 1963 for the Geological Museum of Copenhagen.

Composition and classification

Scientific analysis classifies it as a IIIAB iron, belonging to the chemical group known for its relatively low gallium and germanium content. Its internal structure is that of a medium octahedrite, exhibiting the distinctive Widmanstätten pattern when etched with acid, which forms from the slow cooling of the parent asteroid core over millions of years. The primary metallic phases are kamacite and taenite, with minor inclusions of schreibersite and troilite. This composition is consistent with originating from the differentiated core of a planetesimal that shattered in a catastrophic collision within the asteroid belt long before its encounter with Earth.

Impact and crater

The meteorite struck Earth approximately 10,000 years ago during the Holocene epoch, creating a significant impact event. While no single, large impact crater has been definitively identified, the distribution of fragments over a large strewn field on the Cape York Peninsula in Greenland suggests the main mass broke apart in the atmosphere in a meteoroid procession. The impact energy, estimated to be equivalent to multiple megatons of TNT, would have produced a dramatic air burst and scattered debris across the ice cap and tundra. Research led by scientists from the University of Copenhagen and the Natural History Museum of Denmark continues to study the geomorphology of the region for evidence of associated craterlets or impactite deposits.

Cultural significance

For the Inuit of the Thule region, the meteorite provided a crucial, pre-industrial source of high-quality metal in an environment devoid of native copper or iron ore deposits. The material, known as "Savik", was traded over long distances and cold-hammered into vital tools, ulu blades, and harpoon tips, profoundly influencing the Thule culture and its technological development. This use represents one of the earliest and most sustained documented employments of extraterrestrial material by a human culture. The meteorite's story also intertwines with the era of Arctic exploration, involving figures like Robert Peary and the American Museum of Natural History, highlighting themes of scientific acquisition and colonialism.

Notable fragments

The recovered masses are individually named, with the largest being Ahnighito (also known as "The Tent"), weighing 30.9 tons and displayed in the Arthur Ross Hall of Meteorites at the American Museum of Natural History. Agpalilik ("The Man"), weighing approximately 20 tons, is the centerpiece of the meteorite collection at the Geological Museum of Copenhagen. Other major fragments include The Woman (approx. 3 tons) and The Dog (approx. 400 kg), also in New York City, and Savik I, found near the settlement of Savissivik. The collective study of these pieces by institutions like the Smithsonian Institution and the Max Planck Institute for Chemistry has provided invaluable data on the formation of the early Solar System.

Category:Iron meteorites Category:Meteorites found in Greenland Category:Holocene impact craters