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

Raw translucent chalcedony (likely agate or common opal)

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

AI-generated identification · may be incorrect

Pale blue-gray to honey-yellow, translucent, vitreous to waxy luster, and irregular conchoidal fracture. Chalcedony has Mohs hardness 6.5–7; opal is softer at about 5.5–6.5. No visible cleavage.

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Physical properties

Pale blue-gray to honey-yellow, translucent, vitreous to waxy luster, and irregular conchoidal fracture. Chalcedony has Mohs hardness 6.5–7; opal is softer at about 5.5–6.5. No visible cleavage.

Formation & geological history

Silica-rich groundwater deposited gel or microcrystalline silica in cavities and fractures of volcanic rock, commonly during the Cenozoic or earlier. The yellow color may result from iron staining or natural zoning.

Uses & applications

Used for cabochons, carvings, beads, decorative stone, and lapidary practice; ordinary fragments have little industrial value.

Geological facts

The specimen’s translucent blue body with a yellow edge is consistent with chalcedony or common opal, but the photograph cannot distinguish them definitively. A refractive-index, hardness, or specific-gravity test would help.

Field identification & locations

Look for waxy luster, conchoidal fracture, translucency, and absence of cleavage; quartz will not scratch with a steel knife, while opal may. Common sources include Brazil, Uruguay, Mexico, Australia, and the western United States.