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Petrified Wood is a fossil in which the organic remains have been replaced by minerals in the slow process of turning to stone. This petrification
 process generally results in a Quartz Chalcedony mineralization. Special
 rare conditions must be met in order for the fallen wood to be 
transformed into precious Fossil Wood or Petrified Wood.
 In general, the fallen trees get buried in an environment free of 
oxygen (anaerobic environment), which preserves the original tree 
structure and general appearance. The other conditions include a regular
 access to mineral rich water flowing through the wood, replacing the 
organic tree structure with inorganic stone. The end result is Petrified Wood,
 a tree, with its original basic structure in place, replaced by stone. 
This process could occur in less than one thousand years. Exotic 
minerals allow the rare red and green hues that can be seen in more rare
 specimens.
Fossil Petrified Wood is found in many parts of the world, most commonly perceived to be from Arizona, US. Other significant places known for Petrified Wood
 include Madagascar, Brazil, and Indonesia. Madagascar produces, by far,
 the largest commercial quantity of brown petrified wood sold on the 
world market.
Petrified Wood Skulls
Petrified Wood is a fossil in which the organic remains have been replaced by minerals in the slow process of turning to stone. This petrification
 process generally results in a Quartz Chalcedony mineralization. Special
 rare conditions must be met in order for the fallen wood to be 
transformed into precious Fossil Wood or Petrified Wood.
 In general, the fallen trees get buried in an environment free of 
oxygen (anaerobic environment), which preserves the original tree 
structure and general appearance. The other conditions include a regular
 access to mineral rich water flowing through the wood, replacing the 
organic tree structure with inorganic stone. The end result is Petrified Wood,
 a tree, with its original basic structure in place, replaced by stone. 
This process could occur in less than one thousand years. Exotic 
minerals allow the rare red and green hues that can be seen in more rare
 specimens.
Fossil Petrified Wood is found in many parts of the world, most commonly perceived to be from Arizona, US. Other significant places known for Petrified Wood
 include Madagascar, Brazil, and Indonesia. Madagascar produces, by far,
 the largest commercial quantity of brown petrified wood sold on the 
world market.
Petrified Wood is a fossil in which the organic remains have been replaced by minerals in the slow process of turning to stone. This petrification
 process generally results in a Quartz Chalcedony mineralization. Special
 rare conditions must be met in order for the fallen wood to be 
transformed into precious Fossil Wood or Petrified Wood.
 In general, the fallen trees get buried in an environment free of 
oxygen (anaerobic environment), which preserves the original tree 
structure and general appearance. The other conditions include a regular
 access to mineral rich water flowing through the wood, replacing the 
organic tree structure with inorganic stone. The end result is Petrified Wood,
 a tree, with its original basic structure in place, replaced by stone. 
This process could occur in less than one thousand years. Exotic 
minerals allow the rare red and green hues that can be seen in more rare
 specimens.
Fossil Petrified Wood is found in many parts of the world, most commonly perceived to be from Arizona, US. Other significant places known for Petrified Wood
 include Madagascar, Brazil, and Indonesia. Madagascar produces, by far,
 the largest commercial quantity of brown petrified wood sold on the 
world market.
 
