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How to identify Petrified Wood

Silicified Wood (variety of Chalcedony/Quartz)

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To correctly identify Petrified Wood (Silicified Wood (variety of Chalcedony/Quartz)), 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. 1

    Color

    Overall color and any zoning or banding

    Extremely variable, depending on trace mineral impurities. Common colors include shades of brown, gray, black, red, orange, yellow, and sometimes blue or green. Often exhibits multiple colors in bands or patterns.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous (glassy) to waxy, depending on the specific type of silica (chalcedony or opal) and the polish.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Smooth to slightly granular when broken, but the surface often retains the texture of the original wood, including bark patterns, wood grain, and growth rings. Can feel cool and hard to the touch.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Does not exhibit macroscopic crystal forms; it is a pseudomorph after wood. The silica itself is cryptocrystalline (chalcedony) or amorphous (opal).

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None, as it is composed of cryptocrystalline quartz or opal.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Typically found in sedimentary environments where rapid burial of plant material occurred, often associated with volcanic ash falls, floodplains, ancient riverbeds, and lake deposits. Common in arid or semi-arid regions where erosion exposes ancient sedimentary layers.

Key Facts

Hardness
6.5-7 on the Mohs scale (due to quartz/chalcedony)
Specific Gravity
2.58-2.64 (similar to quartz)
Crystal System
Trigonal (for chalcedony/quartz component), but the overall form is a pseudomorph after wood.
Color
Highly variable, depending on trace elements (e.g., iron oxides for reds/yellows, manganese for blacks/blues).
Luster
Vitreous to waxy
Transparency
Opaque to translucent
Fracture
Conchoidal to splintery
Cleavage
None
Composition
Primarily Silicon Dioxide (SiO2), often with trace impurities of iron, manganese, carbon, copper, chromium, cobalt.

Physical characteristics

  • Crystal Habit: Pseudomorph after wood; cryptocrystalline aggregates (chalcedony) or amorphous (opal).
  • Cleavage Type: None
  • Fracture Type: Conchoidal to splintery
  • Tenacity: Brittle
  • Luster Type: Vitreous to waxy

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