Rock Identifier
Petrified Wood (Silicified wood (primarily Quartz/Chalcedony, SiO2)) — metamorphic
metamorphic

Petrified Wood

Silicified wood (primarily Quartz/Chalcedony, SiO2)

Hardness: 6.5-7 (Mohs); Color: Tan, brown, reddish-brown with visible grain; Luster: Waxy to vitreous; Crystal structure: Microcrystalline (cryptocrystalline); Specific gravity: 2.6-2.9

Hardness
6
Color
Tan, brown, reddish-brown with visible grain
Luster
Waxy to vitreous
Identified More metamorphic

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Physical properties

Hardness: 6.5-7 (Mohs); Color: Tan, brown, reddish-brown with visible grain; Luster: Waxy to vitreous; Crystal structure: Microcrystalline (cryptocrystalline); Specific gravity: 2.6-2.9

Formation & geological history

Formed through permineralization where organic wood materials are replaced by minerals (silica) over millions of years, typically in volcanic ash or sedimentary river deposits; ages range from Devonian to Pleistocene.

Uses & applications

Used for jewelry (cabochons), lapidary art, decorative bookends, furniture tops, and as a popular teaching and collecting specimen.

Geological facts

Arizona's Petrified Forest National Park contains one of the world's largest and most colorful concentrations of petrified wood. It is the state fossil of Arizona and the state stone of Washington.

Field identification & locations

Identify in the field by looking for distinct wood grain patterns, growth rings, or bark textures in a stone that is heavy and cannot be scratched by a steel knife. Common in sedimentary basins with a history of volcanic activity.