H6 Chondrite with Fusion Crust from Algeria

This is a great affordable meteorite.

The H6 chondrite, categorized within the ordinary chondrite group, is a fascinating specimen originating from Algeria. Known for its rich composition of silicate minerals and metallic iron, this meteorite exhibits a unique structure formed under the extreme conditions of space.

This particular H6 chondrite is distinguished by its fusion crust, a thin outer layer that develops during its fiery passage through Earth's atmosphere. The fusion crust appears as a dark, glassy coating, highlighting the meteorite's extraterrestrial journey. The surface often bears a textured appearance, indicative of rapid cooling upon entering the atmosphere.

H6 chondrites are primarily composed of olivine, pyroxene, and metal, and they provide valuable insights into the early solar system's building blocks. The composition of this meteorite reflects conditions in the protoplanetary disk and contributes to our understanding of planetary formation.

The Algerian origin adds to the intrigue of this H6 chondrite, as North Africa has been a notable site for meteorite finds. Collectors and researchers alike value this specimen not only for its scientific significance but also for its striking aesthetic appeal, making it a remarkable addition to any collection.