Rock Identifier
Polished chalcedony with iron-oxide cap (probable carnelian/agate) (Microcrystalline quartz, SiO₂, with hematite/goethite inclusions) — mineral
mineral

Polished chalcedony with iron-oxide cap (probable carnelian/agate)

Microcrystalline quartz, SiO₂, with hematite/goethite inclusions

AI-generated identification · may be incorrect

Gray-blue to reddish-brown, waxy to glassy luster, cryptocrystalline structure, no visible cleavage, conchoidal fracture; Mohs hardness about 6.5–7 and specific gravity near 2.6. The red-brown area likely reflects iron-oxide staining or a separate jasper/carnelian zone.

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Physical properties

Gray-blue to reddish-brown, waxy to glassy luster, cryptocrystalline structure, no visible cleavage, conchoidal fracture; Mohs hardness about 6.5–7 and specific gravity near 2.6. The red-brown area likely reflects iron-oxide staining or a separate jasper/carnelian zone.

Formation & geological history

Forms when silica-rich groundwater fills cavities and fractures in volcanic rock, later incorporating iron oxides; commonly Cenozoic to older, depending on host rock. The smooth surface indicates tumbling or polishing.

Uses & applications

Used for cabochons, beads, carvings, decorative objects, and lapidary practice; attractive color zoning can increase jewelry and collector appeal.

Geological facts

Chalcedony is an aggregate of microscopic quartz crystals rather than a single large crystal. Red coloration commonly comes from hematite or hydrated iron oxides.

Field identification & locations

Likely chalcedony or agate, but the photograph cannot confirm the exact variety. Test for glassy conchoidal fracture and hardness, and inspect translucency; common sources include Brazil, Uruguay, India, Madagascar, and the western United States.