
sedimentary
Petrified Wood
Silicified Wood (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Multi-colored with shades of brown, tan, yellow, and grey; Luster: Waxy or vitreous; Crystal structure: Microcrystalline (Cryptocrystalline) quartz; Cleavage: None; Specific gravity: 2.6-2.9
- Hardness
- 6
- Color
- Multi-colored with shades of brown, tan, yellow, and grey
- Luster
- Waxy or vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Multi-colored with shades of brown, tan, yellow, and grey; Luster: Waxy or vitreous; Crystal structure: Microcrystalline (Cryptocrystalline) quartz; Cleavage: None; Specific gravity: 2.6-2.9
Formation & geological history
Formed via permineralization where organic remains are replaced by minerals (usually silica) through groundwater over millions of years. Most common specimens are from the Triassic, Jurassic, or Cenozoic eras.
Uses & applications
Used primarily for ornamental items, jewelry (cabochons), interior design (tabletops/bookends), and as educational museum specimens.
Geological facts
Even though it is made of stone, the cellular structure of the original tree is often preserved in incredible detail, allowing paleobotanists to identify the species of the ancient tree.
Field identification & locations
Identify in the field by looking for wood-grain patterns, bark textures, or growth rings in a heavy, stony material. Commonly found in arid regions like Arizona (Petrified Forest National Park) and Washington state.
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