Polished Green Epidote, Feldspar and Sparkling Mica Obelisk

Epidote commonly forms elongated, prismatic crystals, which are clearly visible throughout this specimen. These dark green crystal blades intersect at varying angles, giving the obelisk strong visual depth and structure. Mica layers are interspersed between the epidote formations, contributing subtle flashes of reflectivity when viewed from different angles. Lighter mineral zones create contrast against the darker crystalline matrix. The obelisk has been carefully polished to preserve sharp geometry while allowing the internal mineral relationships to remain clearly visible. This piece is well-suited for mineral collectors or as a bold display specimen.