Rock Identifier
Petrified wood (Silicified fossil wood; commonly composed of microcrystalline quartz (SiO₂)) — fossil
fossil

Petrified wood

Silicified fossil wood; commonly composed of microcrystalline quartz (SiO₂)

AI-generated identification · may be incorrect

Wood-grain texture and elongated form are visible. If petrified, hardness is about 7 Mohs, with a vitreous-to-waxy luster and no cleavage; the image alone cannot confirm mineralization or determine color reliably.

Identified More fossil →
Explore Petrified wood in the encyclopedia →

Identify your own rocks.

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

Physical properties

Wood-grain texture and elongated form are visible. If petrified, hardness is about 7 Mohs, with a vitreous-to-waxy luster and no cleavage; the image alone cannot confirm mineralization or determine color reliably.

Formation & geological history

Forms when buried wood is gradually replaced or filled by silica-rich groundwater while retaining its structure. Fossil wood ranges from relatively recent deposits to hundreds of millions of years old; this specimen’s age and locality cannot be determined from the photo.

Uses & applications

Collected and displayed as a fossil; polished pieces are used in lapidary work and décor. It has little structural or industrial use compared with ordinary wood or silica materials.

Geological facts

Petrified wood preserves anatomical details such as growth rings and cellular structure, sometimes at microscopic scale.

Field identification & locations

The grain-like ridges suggest wood, but the pictured piece could also be ordinary weathered wood; petrified wood is heavier and harder than wood and does not splinter or burn like it. Common deposits occur in volcanic-ash-rich sedimentary settings worldwide.