Petrified Wood
Silicified Wood (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 6.5-7 on Mohs scale; Color: Brown, tan, reddish; Luster: Vitreous to dull; Crystal structure: Cryptocrystalline (Microcrystalline Quartz); Cleavage: None/Conchoidal fracture.
Formation & Geological History
Formed through permineralization where organic matter is replaced by silica (typically chalcedony or opal) in an anaerobic environment, often buried under volcanic ash or sediment millions of years ago (Mesozoic to Cenozoic eras).
Uses & Applications
Used in jewelry (lapidary), interior design (tabletops, bookends), and as a popular specimen for geological and fossil collectors.
Geological Facts
Petrified wood is the state fossil of Arizona and Washington. The cell structure of the original tree is often preserved in such detail that the species of the tree can be identified.
Field Identification & Locations
Identify in the field by looking for bark-like textures or growth rings on a stone that is significantly harder and heavier than wood. Common in the Petrified Forest National Park (Arizona) and similar arid sedimentary basins.
Identified on: 5/20/2026
Mode: Standard