This Coyamito Agate halve is a complex geological tapestry encased in its original full husk. The specimen features a blend of medium and irregular banding that creates a vivid depth illusion, making the internal patterns appear to recede into the stone. The face is alive with chromatography, showcasing a rapid transition of colors that weave around sharp eyes and circles. Deep within the quartz-filled core, rare sagenite—fine, needle-like acicular inclusions—radiates through the matrix, accompanied by subtle dotted inclusions. Despite moderate fractures, the flat mirror polish provides a high-clarity view of these intersecting features.