
meteorite
Polished iron meteorite fragment
Iron meteorite, chiefly kamacite and taenite (Fe–Ni alloys), possibly weathered or etched
AI-generated identification · may be incorrectMetallic to dull brown-black luster with rounded fusion-like contours, corrosion pits, and pale inclusions; hardness about 4–5 Mohs, very high density (~7–8 g/cm³), and weak magnetism to strong magnetism.…
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Physical properties
Metallic to dull brown-black luster with rounded fusion-like contours, corrosion pits, and pale inclusions; hardness about 4–5 Mohs, very high density (~7–8 g/cm³), and weak magnetism to strong magnetism. The irregular cavities and rusty surface are consistent with oxidation of iron-rich material, though an image alone cannot confirm extraterrestrial origin.
Formation & geological history
If genuine, it formed in the metallic core of a differentiated asteroid and crystallized billions of years ago, then reached Earth as a meteorite. Similar appearances can also result from terrestrial iron slag or heavily corroded metal, which must be ruled out by testing.
Uses & applications
Meteorites are valued as educational and collectible specimens; iron types are cut, polished, and etched to reveal Widmanstätten patterns. They have no ordinary construction use.
Geological facts
A nickel test, density measurement, and laboratory elemental analysis are important; a clean etched face may show interlocking Widmanstätten bands. Slag commonly contains abundant glassy bubbles and irregular mineral inclusions.
Field identification & locations
Common iron meteorite finds include Campo del Cielo (Argentina), Sikhote-Alin (Russia), and Canyon Diablo (Arizona). Strong magnetism, unusually high density, nickel detection, and absence of uniform industrial vesicles support identification, but laboratory verification is recommended.
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