Rock Identifier
Petrified Wood (Silicified Wood (SiO2)) — mineral
mineral

Petrified Wood

Silicified Wood (SiO2)

Hardness: 6.5-7 (Mohs scale); Color: Brown, grey, tan, cream; Luster: Vitreous to waxy; Crystal structure: Amorphous or cryptocrystalline (Chalcedony/Quartz); Cleavage: None; Specific gravity: 2.6-2.9

Hardness
6
Color
Brown, grey, tan, cream
Luster
Vitreous to waxy
Identified More mineral
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Physical properties

Hardness: 6.5-7 (Mohs scale); Color: Brown, grey, tan, cream; Luster: Vitreous to waxy; Crystal structure: Amorphous or cryptocrystalline (Chalcedony/Quartz); Cleavage: None; Specific gravity: 2.6-2.9

Formation & geological history

Formed through permineralization where organic wood materials are replaced by minerals (usually silica) in anaerobic conditions over millions of years, often by volcanic ash or waterborne sediments.

Uses & applications

Used for ornamental carvings, jewelry (lapidary), furniture (tabletops), and highly valued as geological display specimens.

Geological facts

Petrified wood is a fossil in which the organic remains have been replaced by minerals in the slow process of being turned into stone over a period of many millions of years.

Field identification & locations

Identify by tree-like growth rings, bark-like texture, and superior hardness compared to standard wood. Commonly found in Arizona (USA), Madagascar, and Indonesia.