Eriläbilaskvate

Eriläbilaskvate, also known as Erilä's bilaskvate, is a unique and rare mineral species discovered in the Erilä mine in Finland. It was first identified in 1995 and is named after the mine where it was found. The mineral is characterized by its distinctive crystal structure and chemical composition, which includes elements such as calcium, aluminum, silicon, and oxygen.

Eriläbilaskvate belongs to the group of zeolite minerals, which are known for their porous structure and ability to absorb and release water molecules. This property makes eriläbilaskvate interesting for various scientific and industrial applications, including water purification and catalysis.

The mineral typically forms in low-temperature hydrothermal environments, often associated with other zeolite minerals and secondary minerals. Its occurrence is limited to the Erilä mine, making it a significant geological curiosity and a valuable specimen for mineral collectors.

Despite its rarity, eriläbilaskvate has garnered attention from the mineralogical community due to its unique properties and the specific conditions under which it forms. Ongoing research continues to explore its potential applications and the geological processes that lead to its formation.