Rock Identifier
Polished gray metamorphic pebble, likely marble or quartzite (Uncertain; possibly calcitic marble (CaCO₃) or quartzite (SiO₂) with dark mineral veining) — metamorphic
metamorphic

Polished gray metamorphic pebble, likely marble or quartzite

Uncertain; possibly calcitic marble (CaCO₃) or quartzite (SiO₂) with dark mineral veining

AI-generated identification · may be incorrect

Smooth, rounded, light gray to white with dark gray/black patches and possible metallic-looking inclusions; likely vitreous to dull luster. Hardness would be about 3 for marble or 7 for quartzite; no cleavage is visible.

Identified More metamorphic
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Physical properties

Smooth, rounded, light gray to white with dark gray/black patches and possible metallic-looking inclusions; likely vitreous to dull luster. Hardness would be about 3 for marble or 7 for quartzite; no cleavage is visible.

Formation & geological history

Likely a naturally water-worn and polished fragment of metamorphic rock formed when limestone or quartz-rich sandstone recrystallized during regional or contact metamorphism. Precise geological age and locality cannot be determined from the image.

Uses & applications

Suitable as a decorative or pocket stone, cabochon, or craft specimen; marble may be used in dimension stone, while quartzite is used for aggregate, paving, and countertops.

Geological facts

The apparent dark areas may be mica, amphibole, graphite, or staining rather than metallic ore. A steel scratch test and dilute hydrochloric-acid test can distinguish quartzite from calcitic marble.

Field identification & locations

Commonly found in stream gravels and metamorphic terrains worldwide, including the Alps, Appalachians, India, Brazil, and Scandinavia. Quartzite resists a steel scratch; marble fizzes with acid and is easily scratched.