
meteorite
Possible iron meteorite fragment
Iron meteorite, likely kamacite–taenite alloy
AI-generated identification · may be incorrectDark, irregular metallic-looking fragment; apparent hardness about 4–5.5, high density, opaque, and typically weakly magnetic. The image is too low-resolution to confirm fusion crust, metal grains, or regmaglypts.
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Physical properties
Dark, irregular metallic-looking fragment; apparent hardness about 4–5.5, high density, opaque, and typically weakly magnetic. The image is too low-resolution to confirm fusion crust, metal grains, or regmaglypts.
Formation & geological history
If genuine, it formed in a differentiated asteroid’s metallic core and crystallized billions of years ago, commonly 4.5 billion years old, before landing on Earth. Terrestrial slag or dark iron-rich rock is a more common look-alike.
Uses & applications
Meteorites are primarily collected and studied; iron meteorites may be cut, etched, and displayed. Confirmed specimens can have substantial collector value.
Geological facts
A magnet attraction, clean metallic interior, and Widmanstätten pattern after professional etching support identification; vesicular texture or abundant glassy slag strongly argues against a meteorite.
Field identification & locations
Test with a strong magnet, inspect a fresh cut surface, and measure density; avoid destructive acid tests. Confirmation requires petrographic or elemental analysis, especially because the object may also be slag, basalt, or industrial debris.
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