Epidote appears as elongated, dark green crystal blades scattered throughout the piece, forming intersecting patterns that give the obelisk strong visual movement and depth. Lighter feldspar zones provide contrast against the darker epidote, while fine mica inclusions introduce subtle flashes of reflectivity when viewed from different angles. The obelisk has been carefully polished to preserve sharp geometry while allowing the complex mineral relationships to remain clearly visible, making it an excellent display or collector specimen.
