Dinosaur bone is fossilized biological material in which the original bone structure has been replaced by silica, typically chalcedony or quartz. Collectors look for the distinct honeycomb or cell structure of the cancellous bone preserved in a polished cross-section. It occurs in Mesozoic sedimentary deposits where mineral-rich groundwater permeated the skeletal remains.
Is this dinosaur bone?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch dinosaur bone with a known reference. Dinosaur Bone sits at Mohs 5.5-7, softer than the next harder reference, harder than the previous one.
- 2Name the organismDecide what left the fossil before worrying about the rock. Organism: Dinosaurs. Age: Triassic to the end of the Cretaceous (66 million years ago) for non-avian dinosaurs.
- 3Check the preservationPreservation: Permineralization: minerals fill the pores of bone. That controls the weight, the hardness and how the piece takes a polish.
- 4Read the lusterHold the specimen under a strong light. Luster: waxy.
- 5Match the color rangeCompare against the expected color range: brown, red, black, tan, gray, white.
Often confused with
Dinosaur Bone vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside dinosaur bone
Minerals reported to co-occur with dinosaur bone. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 5.5-7
- Density
- 2.5-2.8 g/cm³
- Luster
- Waxy
- Transparency
- Opaque
- Rarity
- Common
- Uses
- Lapidary, Collector, Ornamental, Display
- Host rock
- sedimentary
- Organism
- Dinosaurs
- Age
- Triassic to the end of the Cretaceous (66 million years ago) for non-avian dinosaurs
- Preservation
- Permineralization: minerals fill the pores of bone
Where rockhounds find dinosaur bone
2 mapped spotsClassic worldwide localities
- Utah
- Colorado
- Wyoming
- Madagascar
- Morocco
Field-hunting tip
Where it forms: sedimentary. If you start seeing quartz, chalcedony, calcite in float, you are in the right ground. In the U.S., the densest reported localities are in Wyoming. Start trip planning there.







