Slúiacelike

Slúiacelike is a rare and unique mineral species discovered in the late 20th century. It was first identified in the Slúia River valley in Slovakia, hence its name. The mineral is characterized by its distinctive greenish-blue color and its crystal structure, which belongs to the monoclinic system. Slúiacelike is primarily composed of copper, iron, and oxygen, with a chemical formula of Cu2FeO3. It is often found in association with other copper minerals, such as malachite and azurite.

The mineral's formation is closely linked to the oxidation of copper-rich deposits, a process that occurs when copper-bearing minerals are exposed to atmospheric conditions. This oxidation leads to the precipitation of various copper minerals, including slúiacelike. The mineral's greenish-blue color is a result of the presence of copper in its structure, which absorbs certain wavelengths of light.

Slúiacelike is not widely known or studied due to its rarity and the limited number of locations where it has been found. However, it holds interest for mineral collectors and researchers studying the geochemical processes involved in the formation of copper minerals. The mineral's unique properties and its association with other copper minerals make it a valuable subject for further study.