A striking Coyamito halve dominated by a bold central pseudomorph formation, where elongated tube-like structures radiate outward in a starburst pattern. Warm amber, honey, and soft cream tones frame the composition, outlined by clean fortification that gives the piece a strong, defined presence. The interior is largely quartz-filled, creating a bright, solid backdrop that contrasts with the darker, more textured core. Stalactite-like forms extend through the center, revealing the original growth replaced over time, adding both direction and energy to the piece. Minor fractures are present but unobtrusive. The combination of radial structure and smooth banding gives this specimen a powerful sense of movement and depth.