Gibeon meteorite was formed in space four billion years ago. It exploded upon entering Earth's atmosphere, landing in the desert of Namibia, Africa in scattered pieces over an area 171 miles long and 62 miles wide.
The Namibian government banned the export of Gibeon meteorite, as any newly discovered pieces are automatically protected as national monuments. This means that any meteorite specimens in circulation are of increasing value and incredibly limited supply. The origin and rarity of each meteorite ring makes it a distinctive piece of art.
Gibeon meteorite features a distinct crystalline structure on its surface, a pattern found only in diamonds and gemstones. This visible crystal structure, or Widmanstatten pattern, was caused by extremely slow cooling of the material in space.
The Widmanstatten pattern will vary slightly between pieces, as will the presence of inclusions. Inclusions are dark spots or tiny holes on the surface of the meteorite that are often traces of metals that, in some cases, do not occur naturally on earth. These inclusions are an important clue to the meteorite's origin and are identifiers of its authenticity.
The acid etching of the meteorite is the last step in the production of the ring. It is here where natural characteristics show themselves.
Despite its natural protection against rust, Gibeon meteorite is primarily composed of iron, so oxidation is always a possibility. Exposure to strong oxidizing agents such as chlorine, bleach, or salt can increase the chance of rusting.