Northwest Africa 16788, aka NWA 16788, is the largest meteorite from Mars ever found on Earth. It weighs 24.67 kg, making it about 70% larger than any other known Martian fragment.

On , it was sold at a Sotheby's auction for $5.3 million.Mars rock found in Niger sells for millions in New York - now the country wants answers Damian Zane, BBC News, 10 August 2025Martian meteorite NWA 16788

History NWA 16788 was found in the Agadez Region of Niger on 90 km west of the Chirfa Oasis, by "a meteorite hunter, whose identity remained undisclosed".https://www.mdpi.com/2571-9408/7/12/323 A small piece of the rock was given to the Shanghai Astronomy Museum to be identified.

It is kept in a private gallery in Arezzo, Italy. Two fragments are kept at the University of Firenze. A sample is also held at the Purple Mountain Observatory in China.

From 8 to , it was on display at Sotheby's in New York before the live auction on , where it was expected to sell for between $2-4 million USD, making it the most valuable meteorite ever auctioned at Sotheby's. It was sold for $5.3 million USD to an anonymous buyer.

Niger has launched an investigation into the circumstances of the discovery, export, and sale of the meteorite. The government "expressed doubts about the legality of its export, raising concerns about possible illicit international trafficking". On , United States Attorney for the District of Columbia Jeanine Pirro announced through her social media channels that the government had seized the meteorite on based on (Aiding unlawful importation) and was preparing a forfeiture action to acquire government title. Authorities had been unable to identify the lawful owner of the meteorite, and according to United States Customs and Border Protection there was no record of importation into the United States.

Description The meteorite is classified as a shergottite. It is 24.665 kg, has a gray to brown surface, and is partly covered with fusion crust that is gray to brownish.

Petrography The surface has a porphyritic texture. There are olivine phenocrysts with a maximum size of 3 mm that are embedded into a groundmass of maskelynite and ophitic pyroxene. These olivine phenocrysts contain partly crystallized melt inclusions, and the inclusions measure tens of micrometers.

There are also minor phases such as merrillite, ilmenite, chromite, and pyrrhotite. Also observable are shock-melted areas.

Geochemistry Olivine phenocrysts: Mg-rich core (Fo73) to a Fe-rich rim (Fo46) Olivine within groundmass: range of Fa35-46 Olivine average Fe/Mn ratio: 49±3 (N=20) Pyroxene: pigeonite (Fs26-31Wo4-8) ranging to augite (Fs18-24Wo22-32) Pyroxene average Fe/Mn ratio: 30±3 (N=17) Maskelynite composition: An49-52Ab46-49Or1-2 (N=4)

See also

Allan Hills 84001 Glossary of meteoritics List of Martian meteorites Nakhla meteorite

References