järkladerine

Järkladerine is a rare and unique mineral discovered in the late 20th century. It was first identified in the Järkliden mine in Sweden, from which it derives its name. The mineral is characterized by its distinctive greenish-blue color and its complex crystal structure. Järkladerine is a member of the zeolite group, which are a class of minerals known for their porous structure and ability to absorb and release water.

The chemical composition of järkladerine is (Na,K)2Ca2(Si12Al4O32)12·12H2O. This formula indicates that the mineral contains sodium, potassium, calcium, silicon, aluminum, oxygen, and water. The presence of water molecules within the crystal structure contributes to its porous nature.

Järkladerine is typically found in low-temperature hydrothermal veins, often associated with other zeolite minerals such as stilbite and heulandite. Its formation is believed to occur under specific geological conditions, including the presence of silica-rich fluids and the interaction with host rocks.

Due to its rarity and the specific conditions required for its formation, järkladerine is not commonly used in industrial applications. However, it is of interest to mineralogists and geologists for its unique properties and the insights it provides into the geological processes that form zeolite minerals. The study of järkladerine continues to contribute to our understanding of mineralogy and geochemistry.