Meteorite Steinbach 0,4g – Germany

Steinbach is one of the most fascinating European meteorites. The first recovered specimens date back to the early 18th century and were found near the village of Steinbach in Saxony. Additional fragments were later discovered in the vicinity of Johanngeorgenstadt and Rittersgrün. The total known weight of the meteorite is approximately 98 kilograms.

Steinbach is classified as an anomalous IVA iron meteorite. It consists primarily of an iron-nickel alloy containing silicate-rich areas composed of olivine, pyroxene, tridymite, and other minerals. The meteorite also contains kamacite, taenite, plessite, chromite, and troilite. This unusual combination of minerals makes Steinbach one of the most remarkable iron meteorites in the world.

For many years, Steinbach was considered a pallasite because it contains translucent olivine crystals embedded within a metallic matrix. Modern mineralogical studies have shown, however, that its silicate portion is not composed solely of olivine but represents a more complex igneous rock containing pyroxene, tridymite, and other minerals. Its structure and formation therefore differ significantly from those of true pallasites, and it is now classified as an anomalous IVA iron meteorite.

When an etched surface is examined, the metallic portion of the meteorite reveals a distinct Widmanstätten pattern formed by kamacite and taenite. Combined with the translucent silicate areas, it creates a unique appearance rarely seen among iron meteorites.

Steinbach is a highly sought-after collector's meteorite. Its historical significance, limited amount of known material, and extraordinary combination of a metallic matrix with silicates make it one of the most desirable European meteorites for collectors and museums.