Rock Identifier
Quartz-rich breccia or druzy quartz specimen (Microcrystalline to crystalline SiO₂, likely quartz/chalcedony with iron-oxide staining and possible host-rock fragments) — mineral
mineral

Quartz-rich breccia or druzy quartz specimen

Microcrystalline to crystalline SiO₂, likely quartz/chalcedony with iron-oxide staining and possible host-rock fragments

AI-generated identification · may be incorrect

Hardness 7 (quartz), white to gray and honey-brown, vitreous to waxy luster, hexagonal quartz structure; generally lacks cleavage and shows irregular fractures. The angular internal pattern suggests brecciation, with sparkling crystal-lined cavities or veins.

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Physical properties

Hardness 7 (quartz), white to gray and honey-brown, vitreous to waxy luster, hexagonal quartz structure; generally lacks cleavage and shows irregular fractures. The angular internal pattern suggests brecciation, with sparkling crystal-lined cavities or veins.

Formation & geological history

Likely formed when silica-rich hydrothermal fluids filled fractures and cavities, later oxidizing iron-bearing material to produce brown coloration. Exact age and locality cannot be determined from the photograph.

Uses & applications

Primarily a collector specimen, lapidary material, or ornamental stone; quartz is also widely used in glass, ceramics, electronics, and construction aggregates.

Geological facts

Iron oxides commonly create the yellow-brown staining seen in quartz specimens. The specimen may be described commercially as quartz breccia, chalcedony breccia, or druzy quartz depending on crystal texture.

Field identification & locations

Identify by its glassy sparkle, hardness, conchoidal fracture, and inability to scratch with a steel knife; vinegar will not fizz. Common sources include hydrothermal veins and volcanic regions worldwide.