Agate's bands grow inward, wall to core
An agate begins as an empty gas bubble in cooling lava. Silica-rich water seeps in and chalcedony — countless microscopic quartz fibres — crystallises on the cavity walls, then layer by layer toward the centre. Because the bands trace the bubble's shape, an angular pocket yields sharp, zig-zag 'fortification' lines like a fort seen from above. The pattern isn't painted on; it is a record of the stone slowly filling itself from the outside in.