This crystal lattice took millions of years to grow
Slice an iron meteorite, polish it, and bathe it in dilute acid, and a lattice of interlocking metal bands appears: the Widmanstatten pattern. It forms only when molten nickel-iron cools at roughly 100 to a few hundred degrees Celsius per million years, slow enough for two alloys, kamacite and taenite, to separate into crystals. No furnace on Earth can fake it; the wide bands mean the metal sat deep inside a slowly cooling asteroid core for ages.