
fossil
Petrified Wood
Silicified Wood (primarily SiO2)
Hardness: 6.5-7 (Mohs). Color: Brown, black, reddish-brown. Luster: Vitreous to waxy (when polished). Crystal system: Hexagonal/Amorphous. Specific gravity: 2.6-2.9. Exhibits wood grain textures.
- Hardness
- 6
- Color
- Brown, black, reddish-brown
- Luster
- Vitreous to waxy (when polished)
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Physical properties
Hardness: 6.5-7 (Mohs). Color: Brown, black, reddish-brown. Luster: Vitreous to waxy (when polished). Crystal system: Hexagonal/Amorphous. Specific gravity: 2.6-2.9. Exhibits wood grain textures.
Formation & geological history
Formed through the process of permineralization where organic wood material is replaced by minerals, typically silica, over millions of years in anaerobic conditions like volcanic ash or waterlogged sediments.
Uses & applications
Used for decorative items, jewelry (cabochons), table tops, and as educational/collector specimens.
Geological facts
Unlike a typical fossil which is an impression, petrified wood is a three-dimensional replacement of the original plant tissue. It can preserve cellular structures so well that the tree species can often be identified.
Field identification & locations
Identify by wood-like grain, bark-like exterior textures, and hardness (it won't be scratched by a steel knife). Commonly found in areas with ancient volcanic activity such as Arizona (USA), Madagascar, and Indonesia.
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