
sedimentary
Petrified Wood
Silicified Wood (SiO2)
Hardness: 6.5-7 Mohs; Color: Tan, brown, gray, occasionally reddish; Luster: Waxy to vitreous; Crystal Structure: Cryptocrystalline (chalcedony/quartz); Cleavage: None; Specific Gravity: 2.6-2.9.
- Hardness
- 6
- Color
- Tan, brown, gray, occasionally reddish
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 Mohs; Color: Tan, brown, gray, occasionally reddish; Luster: Waxy to vitreous; Crystal Structure: Cryptocrystalline (chalcedony/quartz); Cleavage: None; Specific Gravity: 2.6-2.9.
Formation & geological history
Formed through permineralization where organic remains are replaced by minerals (usually silica) while retaining original structure. Often dates from the Triassic to the Tertiary periods in river delta or volcanic ash environments.
Uses & applications
Used in jewelry (cabochons), interior design (tables, bookends), landscaping, and as a popular educational/collector specimen.
Geological facts
Petrified wood is the state fossil of Arizona, Mississippi, and Washington. In some cases, the replacement is so perfect that cell structures and tree rings are visible under a microscope.
Field identification & locations
Identify by looking for bark textures, growth rings, and wood grain in a piece that feels heavy and cold like stone. Common in Arizona (Petrified Forest National Park), Madagascar, and Indonesia.
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