Rock Identifier
Polished dark breccia or gneiss-like rock (Indeterminate polymictic breccia; likely quartz–feldspar–mica rock with iron-oxide staining) — metamorphic
metamorphic

Polished dark breccia or gneiss-like rock

Indeterminate polymictic breccia; likely quartz–feldspar–mica rock with iron-oxide staining

AI-generated identification · may be incorrect

Dark gray-black, rounded and polished, with irregular pale mineral bands and rusty brown staining. Likely Mohs 6–7, vitreous to dull luster, interlocking granular texture, and no obvious cleavage; exact identification requires hardness, streak, and thin-section tests.

Identified More metamorphic
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Physical properties

Dark gray-black, rounded and polished, with irregular pale mineral bands and rusty brown staining. Likely Mohs 6–7, vitreous to dull luster, interlocking granular texture, and no obvious cleavage; exact identification requires hardness, streak, and thin-section tests.

Formation & geological history

The contrasting fragments or bands suggest brecciation and/or strong metamorphic deformation, later cemented or recrystallized by silica-rich material. Its geological age and locality cannot be determined from the photograph.

Uses & applications

Primarily a decorative or collector specimen; comparable rocks may be used as aggregate, facing stone, or polished ornamental material, but this small piece has little industrial value.

Geological facts

The bright metallic-looking flecks may be pyrite, mica, or iron oxides rather than gold. A polished surface can obscure the original texture and make field identification difficult.

Field identification & locations

Look for a strong reaction to a steel file, glassy quartz grains, and a nonmagnetic or weakly magnetic response; a streak test and acid test can help distinguish minerals. Similar dark breccias and metamorphic rocks occur worldwide.