Common Green Opal
Hydrated amorphous silicon dioxide (SiO2·nH2O)
Rock Type: mineral

Physical Properties
Hardness: 5.5-6.5 on Mohs scale; Color: Yellowish-green to lime green; Luster: Waxy to vitreous; Crystal Structure: Amorphous (non-crystalline); Fracture: Conchoidal; Specific Gravity: 1.9-2.3
Formation & Geological History
Formed from the precipitation of silica-rich waters in cavities of volcanic or sedimentary rocks. It is non-precious because it lacks the internal structure to produce play-of-color. Typically Neogene to Quaternary in age for common varieties.
Uses & Applications
Primarily used for lapidary work, decorative carvings, cabochons for jewelry, and as collector specimens.
Geological Facts
Unlike precious opal, common opal does not show 'fire' or iridescence. The green color is often caused by inclusions of iron or nickel silicate minerals, such as nontronite.
Field Identification & Locations
Identified by its waxy luster, conchoidal fracture (curved glass-like breaks), and relative lightness compared to quartz. Common in Australia, Madagascar, and the Western United States. Rough specimens are best identified by their smooth, waxy feel.
Identified on: 5/13/2026
Mode: Standard