Stacked Mangano Lenticular (Pagoda) Calcite Cluster with Fluorescent Core

The calcite crystals grew in a lenticular habit, stacking over time to create the distinctive pagoda-like structure seen throughout the specimen. Smooth, translucent faces contrast with granular micro-crystal zones, giving the cluster visual complexity from every angle. At the core of the formation lies a fluorescent zone that responds under UV light, adding a dramatic secondary display characteristic. When viewed in darkness with UV illumination, the interior glow highlights growth boundaries and internal crystal structure not visible in normal light. The matrix and crystal surfaces show natural mineral textures and subtle tonal variation, emphasizing the specimen’s unaltered geological character. This listing is for the exact specimen shown—an excellent choice for collectors interested in pagoda calcite formations, UV-reactive minerals, and visually dynamic display pieces.