
meteorite
Iron Meteorite
Meteoritic Iron (Fe-Ni alloy)
Hardness: 4-5 on the Mohs scale; Color: Dark brown to silvery gray (often with a weathered exterior patina); Luster: Metallic when freshly cut, dull or earthy when weathered; Crystal Structure: Octahedrite or hexahedrite with Widmanstätten patterns visible on etched surfaces;…
- Hardness
- 4-5 on the Mohs scale
- Luster
- Metallic when freshly cut, dull or earthy when weathered
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Physical properties
Hardness: 4-5 on the Mohs scale; Color: Dark brown to silvery gray (often with a weathered exterior patina); Luster: Metallic when freshly cut, dull or earthy when weathered; Crystal Structure: Octahedrite or hexahedrite with Widmanstätten patterns visible on etched surfaces; Specific Gravity: Heavy, typically 7.5 to 8.0.
Formation & geological history
Formed in the early solar system, approximately 4.5 billion years ago, within the molten cores of differentiated asteroids that were later shattered by impacts.
Uses & applications
Prized by scientific researchers for understanding solar system formation, and highly valued by collectors and museums.
Geological facts
Iron meteorites represent only about 5% of all meteorite falls, yet they make up the majority of finds because they survive atmospheric entry and weathering much better than stony meteorites.
Field identification & locations
Key identifiers include high density (noticeably heavy for its size), magnetic attraction, a fusion crust or regmaglypts (thumbprint-like depressions), and the absence of quartz or silicate minerals.
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