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Petrified Wood Properties Facts and Photos

small trunk section of the mineral petrified wood
Contents

1. Formation of Petrified Wood
2. Petrified Wood Vs Fossilised Wood
3. What is Peanut Wood?
4. Article Photos
5. Our Collection of Petrified Wood

Formation of Petrified Wood

Petrified wood is a type of fossil in which the organic material has been replaced by natural minerals.  The original cell structure however has remained largely intact.

The process known as petrifaction takes place when fallen trees and plants become buried under volcanic ash or sediment.  Due to lack of oxygen the tree or plant is protected and preserved.

As groundwater rich in minerals such as quartz, calcite, pyrite and occasionally opal flows over the organic matter it fills pores and cavities.  When the water dries up the minerals crystallise which creates an internal cast.

Although most of the original organic matter decomposes the cell walls often remain in tact and surround the newly formed crystals.

petrified wood mineral in a museum display cabinet

Petrified wood (clickable image)

Colours in petrified wood are caused by the different minerals.  Red or pink is from hematite.  Shades of yellow orange and brown are from goethite.  Green comes from pure reduced iron also known as native iron and white comes from quartz.  Black is carbon or pyrite and blue and purple come from manganese dioxide.

The process of petrifaction is extremely slow.  It's believed to take around 10,000 years at the very minimum from start to finish.  There is some research to suggest under the right conditions it may take place over a much shorter period of time.  What is known for sure is the slower the process the more precise the replication.

In some cases petrified wood can be an almost exact replica of the original organic matter right down to microscopic levels.  It's not unknown for ring patterns, bark and wood grain of the original tree to be clearly seen.  It can occasionally be so precise the specific variety of tree can be identified. 

It's sometimes believed petrified wood is the original organic matter which has turned to stone but that's not the case.  The organic matter is always replaced by natural minerals.

three slices of polished petrified wood

Petrified wood slices

Petrified Wood Vs Fossilised Wood

The word petrifaction comes from ancient Greek and means 'wood turned into stone'.  The word fossil comes from the Latin 'fossus' meaning 'dug up' or 'buried'.

In English 'petrified' describes a situation where someone is paralysed by fear which causes them to freeze.  The word 'petrified' means to convert or change something into stone.  It comes from the Latin word 'petra' meaning 'rock' or 'stone'.  The origins of the suffix 'fied' is believed to come from the Latin 'facere' meaning to 'make'. 

The terms fossilised wood and petrified wood are often used interchangeably.  Deciphering the difference between the two materials is not easy.

A thread from 2012 that I discovered in The Fossil Forum makes interesting reading and addresses the matter well.

Petrifaction is a form of fossilisation but for the purpose of simplicity, fossilisation tends to be used instead.  In the forum thread one thing that's emphasised is that not all fossils are reinforced or replaced with minerals.  Those which are seem to be classified as fossilised as opposed to petrified.

According to the Oxford dictionary, 'fossil' means "the remains or impression of a prehistoric plant or animal embedded in rock and preserved in petrified form".  It defines 'petrifaction' as "the process by which organic matter exposed to minerals over a long period is transformed into a stony substance".

Although any organism can be petrified, wood, bone and shell are the most common. 

Petrified ammonite fossil on display in London's Natural History Museum 
Petrified ammonite

What is Peanut Wood?

Peanut wood is a distinctive and unusual type of petrified wood that's not particularly well known.

Around one hundred and twenty million years old, most of the world's current supply started life as conifer trees in Western Australia.  As the trees died they were carried away by water and ended up in the sea as driftwood.  They were then attacked by the teredo navalis. Also known as the naval shipworm, this saltwater clam has an appetite for boring through wood.  It has been an extremely destructive pest for as long as there has been wood in the sea.

Once full of boreholes the driftwood sank to the ocean floor and the process of petrifaction began.

Peanut wood gets its name from the distinctive round to oval shaped markings which can resemble peanuts.  

Peanut wood mineral specimen

Peanut wood

Article Photos

The petrified wood at the top and petrified ammonite are on display in London's Natural History Museum.  Photos by Stone Mania.

The second photo is courtesy of Stan Celestian.  Clicking this image redirects to some impressive photos of petrified wood taken by this talented photographer.

The petrified wood slices in the third photo are from our collection.  With the exception of the peanut wood, all photos are clickable and redirect to the original non-compressed image.

Our Collection of Petrified Wood

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