Petrified Wood
Silicified Wood (SiO2)
Rock Type: sedimentary

Physical Properties
Hardness: 6.5-7 (Mohs scale); Color: Dark brown, black, with visible wood grain; Luster: Dull to greasy; Crystal Structure: Cryptocrystalline; Cleavage: None; Specific Gravity: 2.5-2.8.
Formation & Geological History
Formed via permineralization where organic wood material is replaced by silica (usually chalcedony or quartz) over millions of years by being buried in sediment and saturated by groundwater. Often found in deposits from the Triassic to the Cretaceous periods.
Uses & Applications
Used for decorative items, lapidary work (jewelry and cabochons), architectural accents, and as a popular focus for geological collectors.
Geological Facts
Petrified wood is the state fossil of Arizona, North Dakota, and Louisiana. Despite being made of stone, it often preserves the microscopic structure of the original wood perfectly, including tree rings.
Field Identification & Locations
Identify in the field by looking for distinct wood-like bark texture or internal growth rings on an exceptionally heavy, hard stony specimen. Common in arid sedimentary basins like the Petrified Forest National Park region.
Identified on: 5/20/2026
Mode: Standard