Rock Identifier
Polished seam agate with druzy quartz and iron-oxide inclusions (Quartz (SiO₂), chiefly chalcedony with crystalline quartz and iron oxides/hydroxides) — mineral
mineral

Polished seam agate with druzy quartz and iron-oxide inclusions

Quartz (SiO₂), chiefly chalcedony with crystalline quartz and iron oxides/hydroxides

AI-generated identification · may be incorrect

Hardness 6.5–7 Mohs; gray-white chalcedonic rind surrounds rusty orange-brown, metallic-looking inclusions and small sparkling druzy crystals. Waxy to vitreous luster, microcrystalline quartz structure, no obvious cleavage; density about 2.6 g/cm³.

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Physical properties

Hardness 6.5–7 Mohs; gray-white chalcedonic rind surrounds rusty orange-brown, metallic-looking inclusions and small sparkling druzy crystals. Waxy to vitreous luster, microcrystalline quartz structure, no obvious cleavage; density about 2.6 g/cm³.

Formation & geological history

Silica-rich groundwater filled cavities and fractures in volcanic host rock, depositing layered chalcedony followed by quartz; later oxidation produced the iron colors. The specimen’s exact geological age and locality cannot be determined from the photograph.

Uses & applications

Used as a cabochon, polishing stone, lapidary accent, or collector specimen; attractive pieces may be set in jewelry.

Geological facts

The orange-brown material is probably limonite/goethite or hematite, while the glittering patches are drusy quartz. Polishing exposes contrasting internal growth zones and mineralized fractures.

Field identification & locations

Identify by its very hard quartz-rich surface, waxy chalcedony, rounded agate banding, and sparkly quartz pockets; common sources include Brazil, Uruguay, Mexico, India, and the western United States. A locality label or hardness/streak tests would improve identification.