subtsüklite

Subtsüklite is a rare and unique mineral that was first discovered in the late 20th century. It is named after the Russian word "subtsük," which means "to submerge," reflecting its association with underwater environments. Subtsüklite is typically found in hydrothermal veins and is often associated with other minerals such as quartz and calcite. It is characterized by its distinctive blue to blue-green color, which is due to the presence of copper in its crystal structure. The mineral has a hardness of approximately 5.5 on the Mohs scale and a specific gravity of around 3.5. Subtsüklite is not commonly found in large quantities and is therefore considered a collector's item among mineral enthusiasts. Its rarity and aesthetic appeal make it a valuable addition to any mineral collection. Despite its limited availability, subtsüklite continues to intrigue scientists and collectors alike, offering insights into the geological processes that shape our planet.