How to identify Petrified Wood
Petrified Wood (Silicified Wood)
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Open the appTo correctly identify Petrified Wood (Petrified Wood (Silicified Wood)), check each of these features in order. Many rocks and minerals look alike, so cross-reference multiple properties before deciding.
Step-by-step identification
- 1
Color
Overall color and any zoning or banding
Extremely variable, including shades of brown, gray, black, red, orange, yellow, green, blue, and white. Colors are due to trace mineral impurities (e.g., iron oxides for reds/browns, manganese for blacks/blues, copper for greens/blues).
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Vitreous (glassy) to waxy, depending on the specific silica mineral (quartz, chalcedony, or opal).
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Smooth to slightly rough, often exhibiting the texture of the original wood grain, including growth rings, knots, and bark patterns. Can be microcrystalline to cryptocrystalline.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Typically massive, preserving the original woody structure. Microscopic examination reveals fibrous or granular aggregates of quartz, chalcedony, or opal.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
None, as it is composed of cryptocrystalline silica. It exhibits conchoidal fracture.
- 6
Geological Environment
The rock formation and setting where it occurs
Found in sedimentary basins, ancient floodplains, volcanic ash deposits, and areas where rapid burial of plant material occurred, followed by groundwater infiltration rich in dissolved silica. Common in fossil forests and ancient riverbeds.
Key Facts
- Hardness
- 7 (Mohs scale, due to quartz/chalcedony composition)
- Specific Gravity
- 2.60 - 2.65 (similar to quartz)
- Crystal System
- Trigonal (for quartz/chalcedony component)
- Color
- Highly variable, depending on trace mineral impurities (e.g., iron, manganese, copper)
- Luster
- Vitreous to waxy
- Transparency
- Opaque to translucent
- Fracture
- Conchoidal to uneven
- Cleavage
- None
- Composition
- Primarily silicon dioxide (SiO2), often with trace amounts of iron, manganese, carbon, and other elements that impart color.
Physical characteristics
- Crystal Habit: Massive, pseudomorphic after wood; microcrystalline to cryptocrystalline aggregates.
- Cleavage Type: None
- Fracture Type: Conchoidal to uneven
- Tenacity: Brittle
- Luster Type: Vitreous to waxy
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