05/19/2026
Botryoidal chalcedony from Topaz Mountain, Utah is a textbook example.
6 million years ago, gas bubbles in cooling rhyolite left cavities. Silica-rich fluids later filled them layer by layer, creating these bubbly agate formations.
The host rock is famous for topaz + red beryl, but the secondary minerals are just as wild. ( got plenty of that too !)