Iron Meteorite
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GeoFossils is a Global Meteorite Association (GMA) Trusted Business Member #G0127.
Discover our collection of genuine Iron Meteorites, extraordinary remnants of the metallic cores of ancient asteroids that formed during the earliest history of our Solar System over 4.5 billion years ago.
Composed primarily of iron and nickel, iron meteorites are among the most recognisable and durable meteorites. Many reveal the distinctive Widmanstätten pattern when cut and etched, a natural crystal structure that formed as molten metal cooled extremely slowly within the cores of ancient asteroids over millions of years.
Our collection includes authenticated iron meteorites selected for their scientific significance, authenticity and collector appeal. Whether you are starting your first meteorite collection or adding to an established one, these remarkable specimens provide a tangible connection to the formation of our Solar System.
As our collection continues to grow, additional authenticated Iron Meteorites from recognised localities around the world will be added.
An Iron Meteorite is a meteorite composed primarily of iron and nickel that originated within the metallic core of an ancient differentiated asteroid.
Most formed approximately 4.5 to 4.56 billion years ago, making them among the oldest materials available on Earth.
Yes. Due to their high iron and nickel content, most Iron Meteorites are strongly magnetic.
Yes. Like terrestrial iron, Iron Meteorites can oxidise if exposed to moisture for prolonged periods. Storing them in a dry environment will help preserve their condition.
Absolutely. Their durability, distinctive appearance and fascinating origin make Iron Meteorites an excellent choice for both new and experienced collectors.
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