Opentopia Directory Encyclopedia Tools

Petrified wood

Encyclopedia : P : PE : PET : Petrified wood


Petrified log at the Petrified Forest National Park
Enlarge
Petrified log at the Petrified Forest National Park

Petrified wood is a type of fossil: it exists of fossil wood where all the organic materials have been replaced with minerals (most often a silicate, such as quartz), while retaining the original structure of the wood. The petrifaction process has occurred underground, when wood became buried under sediment. Mineral-rich water flowing through the sediment deposited minerals in the plant's cells and as the plant's lignin and cellulose decayed away, a stone cast was formed in its place.

Minerals such as manganese, iron, and copper in the water/mud during the petrification process give petrified wood a variety of color ranges. Quartz crystals are colorless, but when iron is added to the process the crystals become stained with a yellow or red tint.

Following is a list of minerals and related color hues:

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

Petrified wood has a Mohs hardness level of 7, the same as quartz. Materials scientists have been able to make artificial petrified wood recently [link].

Petrified wood is also the state gem of Washington.

Locations

Polished slice of petrified wood
Enlarge
Polished slice of petrified wood

See also

External links

 


From Wikipedia, the Free Encyclopedia. Original article here. Support Wikipedia by contributing or donating.
All text is available under the terms of the GNU Free Documentation License See Wikipedia Copyrights for details.

Search Titles
0123456789
ABCDEFGHIJ
KLMNOPQRST
UVWXYZ?

E-mail this article to:

Personal Message: