
metamorphic
Polished banded stone, likely black marble or banded gneiss
Graphitic banded marble or quartz-feldspar biotite gneiss; exact identification requires testing
AI-generated identification · may be incorrectDark gray-black, elongated and highly polished, with thin pale linear bands and satin-to-glassy luster. Likely hardness 3–7 depending on composition; massive, non-cleavable appearance, with specific gravity roughly 2.7–2.9.
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Physical properties
Dark gray-black, elongated and highly polished, with thin pale linear bands and satin-to-glassy luster. Likely hardness 3–7 depending on composition; massive, non-cleavable appearance, with specific gravity roughly 2.7–2.9.
Formation & geological history
Metamorphism recrystallized carbonate or quartz-feldspar-rich rock under elevated heat and pressure, producing compositional banding; age cannot be determined from the image. The shape is human-polished or tumbled.
Uses & applications
Used as a decorative stone, worry stone, paperweight, lapidary piece, or ornamental carving; not typically valuable as jewelry unless unusually attractive or locally significant.
Geological facts
The pale stripes may be calcite, quartz, or feldspar, while the dark matrix could contain graphite, biotite, amphibole, or pyroxene. A streak, hardness, acid, and magnetism test would distinguish marble from gneiss.
Field identification & locations
Commonly sourced from metamorphic terrains worldwide, including India, Brazil, Scandinavia, and North America. Calcite-rich material fizzes with dilute hydrochloric acid and scratches easily; quartz-rich material resists scratching by steel.
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