Levyne is a rare, hydrous silicate mineral belonging to the zeolite group. It is characterized by a translucent to transparent appearance and typically comes in a variety of pale colors, including white, beige, yellow, blue, and green. Levyne has a vitreous luster and a prismatic crystal habit, often forming thin, elongated or tabular crystals that are usually found as aggregates or in drusy coatings.
In terms of its chemical composition, levyne is an aluminosilicate mineral with the chemical formula (Ca,Na2,K2,Sr, Ba)6.5 [(AlSi7O18)·2H2O]. It is primarily composed of aluminum, silicon, calcium, sodium, potassium, and various trace elements.
Levyne is typically found in cavities and fractures of various rock types, such as basalts and other volcanic rocks. It commonly occurs in association with other zeolite minerals, including stilbite, heulandite, and chabazite.
Due to its relative scarcity and attractive appearance, levyne is often sought after by mineral collectors and enthusiasts. Its intricate crystal formations and delicate colors make it an aesthetically appealing addition to any mineral collection. However, it is important to note that levyne is not widely used in industrial applications and does not possess any significant economic value outside of its mineralogical significance.
