Rock Identifier
Tumbled blue chalcedony (likely agate or common opal) (Microcrystalline quartz, SiO₂; possibly hydrated silica opal, SiO₂·nH₂O) — mineral
mineral

Tumbled blue chalcedony (likely agate or common opal)

Microcrystalline quartz, SiO₂; possibly hydrated silica opal, SiO₂·nH₂O

AI-generated identification · may be incorrect

Smooth, rounded, pale blue-gray, translucent, and waxy to glassy; chalcedony has Mohs hardness 6.5–7, while opal is 5.5–6.5. Quartz varieties are trigonal cryptocrystalline and lack visible cleavage; opal is amorphous.

Identified More mineral
Explore Tumbled blue chalcedony (likely agate or common opal) in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Smooth, rounded, pale blue-gray, translucent, and waxy to glassy; chalcedony has Mohs hardness 6.5–7, while opal is 5.5–6.5. Quartz varieties are trigonal cryptocrystalline and lack visible cleavage; opal is amorphous.

Formation & geological history

Chalcedony forms when silica-rich groundwater fills cavities and fractures, often in volcanic rocks; opal forms from hydrated silica gels. Precise age and identity cannot be determined from the photograph.

Uses & applications

Used for inexpensive jewelry, cabochons, beads, carvings, and collectors’ specimens; industrial chalcedony is occasionally used as a silica source.

Geological facts

The uniform rounded shape and polished surface indicate human tumbling. Blue coloration may be natural, dyed, or enhanced, and color alone cannot reliably distinguish chalcedony from opal.

Field identification & locations

Common sources include Brazil, Uruguay, Madagascar, India, Mexico, and the western United States. A scratch test, specific-gravity test, and close inspection for banding or play-of-color can help; avoid scratching valuable pieces.