
sedimentary
Petrified Wood
Silicified Wood (SiO2)
Hardness: 6.5-7 (Mohs scale); Color: Tan, brown, grey, and cream; Luster: Waxy to vitreous; Crystal structure: Microcrystalline (Cryptocrystalline) quartz; Cleavage: None (conchoidal fracture).
- Hardness
- 6
- Color
- Tan, brown, grey, and cream
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Tan, brown, grey, and cream; Luster: Waxy to vitreous; Crystal structure: Microcrystalline (Cryptocrystalline) quartz; Cleavage: None (conchoidal fracture).
Formation & geological history
Process of permineralization where organic wood material is replaced by minerals, typically silica, after being buried in sediment/volcanic ash. Often millions of years old (frequently Paleozoic to Cenozoic).
Uses & applications
Used for home decor, lapidary arts like bookends and tabletops, jewelry (cabochons), and as museum or collector specimens.
Geological facts
Sometimes the replacement is so perfect that cell structures and tree rings are visible under a microscope. Arizona's Petrified Forest National Park contains one of the world's largest concentrations of it.
Field identification & locations
Identify in the field by looking for wood-like textures (bark, rings) combined with a stony, heavy, and hard surface that cannot be scratched by a steel pocketknife. Common in sedimentary basins.
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