Rock Identifier
Fossiliferous wood / petrified wood fragment (Silicified or partially mineralized wood (fossil wood; commonly quartz/chalcedony replacement)) — fossil
fossil

Fossiliferous wood / petrified wood fragment

Silicified or partially mineralized wood (fossil wood; commonly quartz/chalcedony replacement)

AI-generated identification · may be incorrect

Brown-tan, layered woody grain and fibrous texture are visible; luster is dull to subvitreous, with no obvious cleavage. Typical hardness is about 6.5–7 if fully silicified, but this specimen appears partly weathered and may be softer; specific gravity commonly 2.2–2.7.

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Physical properties

Brown-tan, layered woody grain and fibrous texture are visible; luster is dull to subvitreous, with no obvious cleavage. Typical hardness is about 6.5–7 if fully silicified, but this specimen appears partly weathered and may be softer; specific gravity commonly 2.2–2.7.

Formation & geological history

Buried wood was preserved and gradually replaced by silica-rich groundwater, often during the Cenozoic or late Mesozoic; exact age cannot be determined from the photograph. It commonly forms in volcanic ash beds, river deposits, and sedimentary basins.

Uses & applications

Collected as a fossil and used for polished slabs, cabochons, bookends, and decorative objects; it has little construction value in fragment form.

Geological facts

The best identification clue is preserved cellular or growth-ring structure rather than ordinary sedimentary layering. Complete silicification can preserve microscopic wood anatomy in remarkable detail.

Field identification & locations

Common localities include Arizona, Colorado, Oregon, Madagascar, Indonesia, and Australia. Look for wood grain, cell patterns, a glassy fracture, and inability to scratch it with a steel knife; acid testing is generally unhelpful.