Exceptional 60.35 g Martian meteorite officially classified as a poikilitic shergottite. This substantial end cut reveals a spectacular crystalline texture with strong contrast between dark pyroxenes and lighter silicates, offering a remarkable view into the geology of Mars. A rare and highly collectible specimen from the limited NWA 13925 find.
This 60.35 g end cut of NWA 13925 is an authentic Martian meteorite officially classified as a shergottite in the Meteoritical Bulletin. Its large polished surface offers an exceptional exposure of the meteorite’s internal structure, revealing the coarse crystalline texture characteristic of certain Martian igneous rocks.
Martian meteorites are among the rarest meteorites known on Earth, originating from the crust of Mars before being ejected into space by massive asteroid impacts.
The cut face displays a striking poikilitic texture composed of dark pyroxenes contrasting with lighter silicate-rich areas. This natural mineralogical pattern gives the specimen remarkable visual depth and immediately distinguishes it from ordinary meteorites.
The irregular contour of the specimen preserves part of the natural exterior while maximizing the visible interior structure, making this end cut particularly aesthetic for display.
NWA 13925 was officially classified as a Martian meteorite in Meteoritical Bulletin 110. Scientific analysis identified minerals including olivine, pyroxenes, maskelynite, chromite, ilmenite, merrillite, and pyrrhotite. The meteorite exhibits a poikilitic texture typical of certain Martian shergottites.
The classification was carried out by Anthony Irving and Paul Carpenter, both internationally recognized experts in planetary meteorites.
With a total known weight of only 1250 g, NWA 13925 remains an extremely limited Martian meteorite. Specimens of this size offering such a large exposed surface are particularly desirable for advanced collectors, museums, and educational displays.
This specimen provides a direct connection to Mars through genuine volcanic material formed on another planet billions of years ago.
Yes. NWA 13925 is officially classified in the Meteoritical Bulletin as a Martian shergottite.
A poikilitic shergottite is a Martian igneous meteorite where large pyroxene crystals enclose smaller mineral grains, producing a distinctive coarse crystalline texture.
Only a very small number of meteorites are confirmed to originate from Mars, making them among the most prestigious meteorites for collectors.
An end cut preserves part of the natural exterior of the meteorite while exposing a polished interior surface revealing its mineralogy and internal structure.
