What you're looking at was once literally living bone tissue from a dinosaur that walked what's now the American West roughly 150 million years ago.
Over that stretch of time, groundwater carrying dissolved silica seeped into the bone's naturally porous structure and gradually replaced it, cell by cell, with agate, chalcedony, or jasper, a process called permineralization.
The web-like, honeycomb pattern you see across each polished surface isn't decorative, it's the actual preserved cellular structure of the original bone, frozen in mineral form.
Material like this comes almost exclusively from the Morrison Formation, a Late Jurassic rock layer spanning parts of Utah and Colorado that's produced some of the most famous dinosaur skeletons ever found, Allosaurus, Stegosaurus, Diplodocus, and Brachiosaurus among them.
Worth knowing honestly upfront: not every bone fragment from this formation turns gem-quality, most fossilized bone recovered is dull grey and holds no lapidary value, only a small percentage silicifies with the color and clarity needed for cutting.
And while the cellular pattern is genuine and identifiable, it's generally not possible to trace a specific cabochon back to a named dinosaur species from the pattern alone, small, dense cell structures usually point away from large theropods, but that's about as specific as identification gets.
Each cabochon here is cut mix shape with a flat back, and colors range from deep reds and browns to occasional blacks and purples depending on which trace minerals were present during fossilization.
In spiritual traditions, dinosaur bone is sometimes associated with grounding and a tangible connection to deep time, fitting for a stone that's quite literally older than most geological concepts of "ancient."