
metamorphic
Tumbled gray-and-white stone, likely quartz-rich marble or quartzite
Quartz (SiO₂)–calcite marble or quartzite; exact identification requires testing
AI-generated identification · may be incorrectHardness likely Mohs 3–7 depending on composition; gray-white, opaque, with a polished/waxy luster and irregular veining. Quartzite is granular and very hard, while marble is calcite-rich and softer, often reacting with dilute acid.
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Physical properties
Hardness likely Mohs 3–7 depending on composition; gray-white, opaque, with a polished/waxy luster and irregular veining. Quartzite is granular and very hard, while marble is calcite-rich and softer, often reacting with dilute acid.
Formation & geological history
Formed when limestone or quartz-rich sandstone underwent metamorphism under heat and pressure; age varies widely by source locality. The rounded shape is human-tumbled and polished.
Uses & applications
Used as a decorative pebble, lapidary material, aggregate, and occasionally architectural stone; generally low jewelry value unless unusually patterned.
Geological facts
The image alone cannot reliably distinguish marble from quartzite. A steel knife scratches marble but not quartzite; vinegar or dilute hydrochloric acid fizzes on exposed calcite.
Field identification & locations
Commonly found in metamorphic belts worldwide, including the Alps, Appalachians, India, Brazil, and Madagascar. Examine grain texture, test hardness, and check acid reaction on an inconspicuous spot.
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