
sedimentary
Petrified Wood
Silicified Wood (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Brown, tan, reddish-brown; Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None; Specific Gravity: 2.6-2.9
- Hardness
- 6
- Color
- Brown, tan, reddish-brown
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Brown, tan, reddish-brown; Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None; Specific Gravity: 2.6-2.9
Formation & geological history
Formed via permineralization where organic wood materials are replaced by minerals (usually silica) while retaining original structure; typically dates from the Devonian to Holocene periods in low-oxygen burial environments.
Uses & applications
Used extensively in jewelry (cabochons), interior design (furniture, bookends), and as highly collectible ornamental specimens.
Geological facts
It is the state fossil of Arizona. Some specimens are so perfectly preserved that tree rings and cellular structures can still be observed under a microscope.
Field identification & locations
Identified by wood-like grain patterns, knots, or bark texture in a stony/glassy material; commonly found in the Petrified Forest National Park (AZ) and various riverbeds or sedimentary basins.
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