This specimen features a striking cluster of ferruginous quartz crystals, characterized by intense red to reddish-brown coloration caused by iron oxide (hematite). The crystals are well-formed, with sharp prismatic shapes and lustrous, transparent to translucent faces that reveal internal iron staining and phantoms. The group is attractively composed, with multiple intergrown quartz points emerging from a white quartz matrix, creating strong contrast between the fiery red crystals and the lighter base. The ferruginous coloration is natural and evenly distributed, enhancing both the aesthetic appeal and the mineralogical interest.