Rock Identifier
Petrified wood (possible) (Silicified wood; fossilized tree tissue, commonly replaced by microcrystalline quartz (SiO₂)) — fossil
fossil

Petrified wood (possible)

Silicified wood; fossilized tree tissue, commonly replaced by microcrystalline quartz (SiO₂)

AI-generated identification · may be incorrect

Tan, cream, and pale gray, with a rough, weathered surface and possible preserved wood grain. If silicified, hardness is about 7 Mohs and luster ranges from dull to waxy; the image alone does not confirm mineral replacement or wood structure.

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Physical properties

Tan, cream, and pale gray, with a rough, weathered surface and possible preserved wood grain. If silicified, hardness is about 7 Mohs and luster ranges from dull to waxy; the image alone does not confirm mineral replacement or wood structure.

Formation & geological history

Forms when buried wood is gradually mineralized, often by silica-rich groundwater. Fossilization can occur across many geological periods; the specimen’s age and origin cannot be determined from the photo.

Uses & applications

Collected as a fossil or display piece; polished silicified wood is also used for ornaments and lapidary work.

Geological facts

Petrified wood preserves the shape and sometimes cellular structure of ancient trees, while the original organic material is largely replaced by minerals.

Field identification & locations

The long, log-like shape suggests petrified wood, but visible growth rings or grain and a hard, stone-like texture would help verify it. Common deposits occur in the western United States and other regions worldwide.