
metamorphic
Banded river pebble, likely quartzite or metamorphosed sandstone
Quartzite (quartz-rich metamorphic rock), possibly banded sandstone
AI-generated identification · may be incorrectFine-grained, rounded and naturally smoothed; pale gray, pink, and brown parallel bands with a dull to subtly sparkling luster. Quartzite is typically Mohs 7, has no cleavage, and a specific gravity near 2.6–2.7.
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Physical properties
Fine-grained, rounded and naturally smoothed; pale gray, pink, and brown parallel bands with a dull to subtly sparkling luster. Quartzite is typically Mohs 7, has no cleavage, and a specific gravity near 2.6–2.7.
Formation & geological history
Formed when quartz-rich sandstone was buried and recrystallized under heat and pressure, preserving sedimentary layering; age cannot be determined from the image. Its rounded shape indicates later abrasion in a river, beach, or glacial setting.
Uses & applications
Primarily a decorative or collectible pebble; quartzite is also used as crushed stone, building stone, and aggregate, though this small specimen has no practical industrial value.
Geological facts
The specimen’s stripes may represent original sedimentary layers or mineral-rich bands. A glass-scratch test and examination of a fresh edge can help distinguish quartzite from softer sandstone.
Field identification & locations
Common in river gravels and glacial deposits worldwide, especially near quartz-rich mountain belts. Quartzite should resist scratching by a steel knife and commonly scratches glass; sandstone is usually more porous and visibly granular.
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