lisandjärelt

Lisandjärelt is a rare and unique mineral that was first discovered in the late 20th century. It is named after the Finnish word "lisäntä", which translates to "addition", reflecting the mineral's unusual chemical composition. Lisandjärelt is typically found in granitic pegmatites, which are igneous rocks formed from the slow crystallization of magma. The mineral is characterized by its distinctive prismatic crystals, which can grow to significant sizes, and its vibrant blue color, which is a result of the presence of copper in its structure.

The chemical formula of lisandjärelt is (Na,K)2Cu(SO4)2·2H2O. This formula indicates that the mineral is a sulfate, with sodium and potassium as the dominant cations, copper as the transition metal, and water molecules as part of its structure. The presence of copper gives lisandjärelt its characteristic blue color, which can range from light blue to deep indigo, depending on the specific conditions of its formation.

Lisandjärelt is of interest to mineralogists and collectors due to its rarity and unique properties. It is also studied for its potential applications in materials science, as its structure and composition make it a candidate for use in the development of new materials with unique properties. Despite its rarity, lisandjärelt is not considered a valuable gemstone due to its softness and tendency to weather and dissolve in water. However, it remains an important and fascinating subject of study in the field of mineralogy.