meteorite

Likely iron meteorite

Iron meteorite, predominantly kamacite and taenite (Fe–Ni alloys)

AI-generated identification · may be incorrect

Gray metallic luster with a rounded, possibly fusion-crusted surface; typical iron meteorites have Mohs hardness about 4–5, density 7.3–7.8, and no cleavage. The image is blurred, so texture and composition cannot be confirmed visually.

Identified September 6, 2026More meteorite →

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Physical properties

Formation & geological history

Formed in the metallic cores of differentiated asteroids, then excavated by impacts and delivered to Earth; most are billions of years old. The smooth shape may reflect atmospheric ablation or terrestrial weathering, but could also be industrial metal.

Uses & applications

Meteorites are valued as collectibles, research specimens, and jewelry material; iron meteorites are occasionally cut, polished, and etched to reveal Widmanstätten patterns.

Geological facts

A genuine iron meteorite commonly attracts a strong magnet and shows a nickel-rich composition; an etched slice may display interlocking crystalline patterns. Slag, cast iron, and rusty industrial metal are frequent look-alikes.

Field identification & locations

Test magnetism, measure unusually high density, inspect for a thin fusion crust, and seek laboratory nickel analysis; a professional meteorite classification is essential. Common finds include Antarctica, Northwest Africa, Australia, and the American Southwest.