
sedimentary
Petrified Wood / Red Jasper
Silicified wood (primarily Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs); Color: Red, brown, tan; Luster: Waxy to vitreous; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.9
- Hardness
- 6
- Color
- Red, brown, tan
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Red, brown, tan; Luster: Waxy to vitreous; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.9
Formation & geological history
Formed through permineralization where organic wood materials are replaced by silica (chalcedony or quartz) over millions of years, often in volcanic ash or sedimentary fluvial environments.
Uses & applications
Used primarily for lapidary work, jewelry (cabochons), interior decor, and as educational geological specimens.
Geological facts
The red coloring is typically due to iron oxide (hematite) impurities during the fossilization process. Petrified wood is the state gem of Washington and the state fossil of Arizona.
Field identification & locations
Identify by looking for preserved wood grain, bark textures, or ring patterns. Field identification is aided by its high hardness (it will scratch glass) and waxy luster when broken.
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