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Petrified wood

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The image shows the center of a polished slice of a petrified tree from Arizona. After the enlargement of the image it is possible to see the remains of insects deep in the tree that lived approximately 230 million years ago in the late Triassic
Petrified log at the Petrified Forest National Park
Polished Petrified Wood
Polished slice of petrified wood
Petrified logs
The outline of cells visible in a segment of petrified wood
Petrified stump exposed at low tide on Ynyslas beach, Wales

Petrified wood (from the Greek root petro meaning "rock" or "stone"; literally "wood turned into stone") is the name given to a special type of fossilized remains of terrestrial vegetation. It is the result of a tree having turned completely into stone by the process of permineralization. All the organic materials have been replaced with minerals (mostly a silicate, such as quartz), while retaining the original structure of the wood. Unlike other types of fossils which are typically impressions or compressions, petrified wood is a three dimensional representation of the original organic material. The petrifaction process occurs underground, when wood becomes buried under sediment and is initially preserved due to a lack of oxygen which inhibits aerobic decomposition. Mineral-laden water flowing through the sediment deposits minerals in the plant's cells and as the plant's lignin and cellulose decay, a stone mould forms in its place.

In general, wood takes less than 100 years to petrify. The organic matter needs to become petrified before it decomposes completely.[1] A forest where the wood has petrified becomes known as a Petrified Forest.

Elements

Elements such as manganese, iron and copper in the water/mud during the petrification process give petrified wood a variety of color ranges. Pure quartz crystals are colorless, but when contaminants are added to the process the crystals take on a yellow, red, and other tint.

Following is a list of contaminating elements and related color hues:

Petrified wood can preserve the original structure of the wood in all its detail, down to the microscopic level. Structures such as tree rings and the various tissues are often observed features.

Petrified wood has a Mohs hardness of 7, the same as quartz crystal.

Petrified wood is the provincial stone of Alberta and also the state gem of Washington.

Locations

Artificial petrified wood

Artificial petrified wood has been produced in a Washington laboratory. In the process small cubes of pine were soaked in an acid bath for two days, then in a silica solution for another two. The product was then cooked at 1400 °C in an argon atmosphere for two hours. The result was silicon carbide ceramic which preserved the intricate cell structure of the wood.[9][10] Soaking in a tungsten solution produced a tungsten carbide petrified wood. [citation needed]

See also

References

  1. ^ Petrified Forest National Park - Frequently Asked Questions from the U.S. National Park Service
  2. ^ http://www.lachlanhunter.deadsetfreestuff.com/JB/Big-Trees/big-trees6.htm
  3. ^ "A petrified forrest near Hoegaarden".
  4. ^ Petrified trees and the forest region (Brazil).
  5. ^ Anon. "The Petrified Forest of Puyango". Viva travel guides. Viva. Retrieved 26 January 2010.
  6. ^ http://bio.kuleuven.be/sys/iawa/PDF/IAWA%20J%2021-25/24%20(2)%202003/24(2)%20163-172.pdf
  7. ^ Fossils: The Other Ancient Egypt
  8. ^ Campbell, J.A. (29 March 1979). "Radiocarbon measurements on submerged forest floating chronologies". Nature. 278 (5703). Nature Publishing Group: 409–413. doi:10.1038/278409a0. Retrieved 12 January 2010. {{cite journal}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  9. ^ Petrified Wood in Days, Physorg.com, January 25, 2005 http://www.physorg.com/news2801.html
  10. ^ Presto! Instant Petrified Wood Created in Lab, Live Science, 27 January 2005 http://www.livescience.com/technology/050127_petrified_wood.html