description Stilbite Overview
Stilbite is a group of hydrated calcium and sodium aluminosilicate minerals in the zeolite family. It commonly forms pale, glassy crystals arranged in sheaf-like, fan-shaped, or bow-tie aggregates, which makes it popular with mineral collectors. Stilbite occurs in cavities and veins of volcanic rocks, especially basalt, where it forms from mineral-rich fluids. The name comes from the Greek word meaning "to shine," referring to the mineral's luster.
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