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Peanut Wood Jasper

Sedimentary (Silicified Fossil Wood)

Silicified fossil wood (Jasper variety)

Also known as: Peanut Wood

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Description

Peanut Wood Jasper is a unique form of petrified wood characterized by distinctive oval or 'peanut-shaped' markings. These markings are fossilized borings made by marine bivalves (often referred to as 'shipworms' or Teredo worms) into driftwood before it became silicified. The wood itself is typically silicified into a dark jasper or chalcedony, ranging from black to dark brown, while the borings are filled with lighter-colored silica, often white, cream, or tan, creating a striking contrast. It is a pseudomorph after wood, meaning the original organic structure has been replaced by mineral matter while retaining the original form.

How to Identify

Color
Dominantly dark brown to black matrix with contrasting white, cream, or tan 'peanut-shaped' inclusions. Other colors like reddish-brown or grey may also be present in the matrix.
Luster
Dull to waxy or vitreous when polished.
Texture
Fine-grained, dense, and smooth when polished. The 'peanut' inclusions may have a slightly different texture or sheen.
Crystal Form
Cryptocrystalline, meaning individual crystals are too small to be seen without high magnification. It retains the macroscopic structure of the original wood.
Cleavage
None, as it is a cryptocrystalline aggregate of quartz.
Geological Environment
Marine sedimentary environments where driftwood was infested by marine borers and subsequently buried and silicified. Often found in ancient marine deposits.

Key Facts

  • Hardness: 6.5-7 on the Mohs scale
  • Specific Gravity: 2.58-2.64
  • Crystal System: Trigonal (as cryptocrystalline quartz)
  • Color: Dark brown to black matrix with white, cream, or tan 'peanut' inclusions
  • Luster: Dull to waxy, vitreous when polished
  • Transparency: Opaque
  • Fracture: Conchoidal to splintery
  • Cleavage: None
  • Composition: Silicon dioxide (SiO2) with various impurities

Quick Check

  • Color: Dark brown to black with white/cream 'peanut' patterns
  • Luster: Dull to waxy
  • Streak: White

Physical Characteristics

  • Crystal Habit: Massive, cryptocrystalline aggregate, pseudomorph after wood
  • Cleavage Type: None
  • Fracture Type: Conchoidal to splintery
  • Tenacity: Brittle
  • Luster Type: Dull to waxy

Formation

Peanut Wood Jasper forms when ancient wood, primarily from the Araucaria tree species, is buried in marine sediments. The wood undergoes permineralization, where organic material is replaced by silica (SiO2) from groundwater. The characteristic 'peanut' patterns are formed by borings of marine bivalves (Teredo worms) into the driftwood before silicification. These borings are subsequently filled with lighter-colored silica or chalcedony, contrasting with the darker, often black or brown, silicified wood matrix.

Usage

Primarily used as an ornamental stone, for lapidary work (cabochons, spheres, carvings), and in jewelry. It is also collected by fossil and mineral enthusiasts due to its unique aesthetic and paleontological significance.

Age Distribution

Cretaceous Period (approximately 120 million years old)

Where to Find

Western Australia

The primary and most well-known source of Peanut Wood Jasper is the Kennedy Range in Western Australia, particularly from the Cretaceous Birdrong Shale formation. It is often found as river-worn pebbles and cobbles.

Finding Tips

Look for distinctive patterns

The most defining characteristic is the 'peanut' or oval-shaped markings against a darker background. These are unmistakable once recognized.

Check for hardness

As a form of jasper (quartz), it will be hard (Mohs 6.5-7) and will scratch glass.

Examine for wood grain

Even though it's silicified, faint remnants of the original wood grain might be visible in the darker matrix, especially on unpolished surfaces.

Consider the geological context

It is found in ancient marine sedimentary environments, often associated with shale or sandstone formations that once contained driftwood.

Similar Rocks

Petrified Wood

Silicified Wood

Also known as: Fossilized Wood

Jasper

Cryptocrystalline Quartz

Also known as: Chert, Agate

Opalized Wood

Opal (SiO2·nH2O) pseudomorph after wood

Also known as: Fossilized Wood (Opal)

Scientific Classification

Mineral Class
Silicates (Tectosilicates)
Group
Quartz Group
Crystal System
Trigonal
Chemical Formula
SiO2
Composition
Silicon dioxide (SiO2) with trace impurities (e.g., iron oxides, organic matter) that impart color. The 'peanut' inclusions are also SiO2, often chalcedony.

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