magamiteid

Magamiteid is a rare and distinctive mineral species discovered in the late 20th century. It is named after the Magamiteid mine in Norway, where it was first found. Magamiteid is characterized by its unique crystal structure and vibrant blue color, which is a result of the presence of copper and iron within its lattice. The mineral belongs to the triclinic crystal system and typically forms as small, prismatic crystals or granular aggregates.

Magamiteid is relatively soft, with a Mohs hardness of approximately 4.5, and has a specific gravity of around 4.1. It exhibits a submetallic luster and a perfect cleavage in one direction. The mineral is often associated with other copper-bearing minerals such as chalcopyrite and bornite, and it can be found in hydrothermal veins and skarn deposits.

Despite its rarity, magamiteid has garnered interest among mineral collectors and researchers due to its distinctive appearance and the scientific insights it provides into the formation of copper-rich minerals. Its discovery has contributed to the ongoing study of mineralogy and geochemistry, particularly in understanding the processes that lead to the formation of unique mineral species in specific geological environments.