Rock Identifier
Fossil Bone Fragment (Fossilized osteological material (Hydroxylapatite permineralized with secondary minerals)) — fossil
fossil

Fossil Bone Fragment

Fossilized osteological material (Hydroxylapatite permineralized with secondary minerals)

AI-generated identification · may be incorrect

Hardness 4-5 on the Mohs scale, earthy to dull luster, grayish-tan color, exhibiting a dense outer cortex and porous inner trabecular structure.

Identified More fossil →
Explore Fossil Bone Fragment in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness 4-5 on the Mohs scale, earthy to dull luster, grayish-tan color, exhibiting a dense outer cortex and porous inner trabecular structure.

Formation & geological history

Formed via permineralization where groundwater minerals deposit into the porous cellular spaces of buried skeletal remains over thousands to millions of years.

Uses & applications

Valued primarily for paleontological study, educational reference collections, and amateur fossil collecting.

Geological facts

Fossil bones readily stick to the tongue due to their microscopic porous structures absorbing moisture, a common field test used by paleontologists.

Field identification & locations

Identified by the distinct honeycombed cancellous bone visible at fractures; typically found in sedimentary formations, river gravels, and badlands.