Viimistulite
Viimistulite is a rare mineral belonging to the silicate group, specifically classified as a sorosilicate. It was first discovered in 1986 in the Viimsi quarry, Estonia, from which it derives its name. The mineral is typically found in contact metamorphic rocks, often associated with skarn deposits. Viimistulite is characterized by its unique crystal structure, which is monoclinic, and its distinctive color, ranging from light yellow to brownish yellow.
The chemical formula of viimistulite is Ca2Mg2Si2O7. It consists of calcium, magnesium, silicon, and oxygen, with
Viimistulite is not commonly found in large quantities and is often collected by mineral enthusiasts for its