
sedimentary
Dinosaur Bone (Gembone)
Petrified Dinosaur Bone (Apatite/Silica replacement)
AI-generated identification · may be incorrectHardness: 6.5–7 on Mohs scale; Color: Dark brown, tan, and black with visible cellular web-like patterns; Luster: Vitreous to waxy (when polished); Structure: Cryptocrystalline replacement of spongy bone tissue; Specific Gravity: 2.6–2.7.
- Hardness
- 6
- Luster
- Vitreous to waxy (when polished)
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Physical properties
Hardness: 6.5–7 on Mohs scale; Color: Dark brown, tan, and black with visible cellular web-like patterns; Luster: Vitreous to waxy (when polished); Structure: Cryptocrystalline replacement of spongy bone tissue; Specific Gravity: 2.6–2.7.
Formation & geological history
Formed through permineralization where minerals (usually silica) leach into the porous spaces of bone. Most gembone in the USA dates to the Jurassic period (approx. 150 million years ago), specifically from the Morrison Formation.
Uses & applications
Primarily used in high-end lapidary work, jewelry (cabochons), and as scientific or investment specimens for fossil collectors.
Geological facts
Gembone is considered one of the rarest fossil materials in the world because it requires specific geological conditions to agatize cells without crushing the bone. Famous specimens often retain the original biological 'marrow' structure in vibrant colors.
Field identification & locations
Identify by looking for the 'honeycomb' or 'cell' pattern characteristic of trabecular (spongy) bone. In the field, look for weathered, petrified fragments with a porous texture in known fossil-bearing strata like those in Utah, Colorado, and Wyoming.
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