redusoivana

Redusoivana is a rare and unique mineral species discovered in the late 20th century. It was first identified in the Red Mountain mine in the state of Nevada, United States, hence its name. The mineral is characterized by its vibrant red color, which is attributed to the presence of iron oxide within its crystal structure. Redusoivana typically forms as small, prismatic crystals or as granular aggregates, often associated with other secondary minerals such as malachite and azurite.

The chemical composition of redusoivana is complex, consisting primarily of copper, iron, and oxygen, with smaller amounts of other elements like sulfur and chlorine. Its crystal system is monoclinic, and it exhibits a distinct cleavage along specific planes. The mineral's hardness on the Mohs scale is approximately 3.5, making it relatively soft and susceptible to scratching.

Redusoivana is of interest to mineralogists and collectors due to its rarity and aesthetic appeal. Its vibrant red color sets it apart from many other minerals, and its association with other secondary minerals adds to its geological significance. Despite its rarity, redusoivana has been found in only a few locations worldwide, primarily in copper-rich deposits. Its discovery and study contribute to the broader understanding of mineral formation processes and the geological history of the regions where it is found.