
metamorphic
Light-colored metamorphic rock, likely quartzite
Quartzite, composed predominantly of recrystallized quartz (SiO₂)
AI-generated identification · may be incorrectPale tan to gray, granular and nonmetallic with a rough surface; quartz has Mohs hardness 7 and a trigonal crystal structure, but individual grains are not clearly visible. The image alone cannot confirm its identity or reliably assess cleavage or density.
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Physical properties
Pale tan to gray, granular and nonmetallic with a rough surface; quartz has Mohs hardness 7 and a trigonal crystal structure, but individual grains are not clearly visible. The image alone cannot confirm its identity or reliably assess cleavage or density.
Formation & geological history
Quartzite forms when quartz-rich sandstone is recrystallized by heat and pressure during metamorphism; its age depends on the original sandstone and later metamorphic event.
Uses & applications
Used as building and decorative stone, aggregate, and, when attractive, in landscaping or collections.
Geological facts
Quartzite is generally harder and more resistant to weathering than its sandstone precursor.
Field identification & locations
Look for fused-looking quartz grains and a scratch-resistant surface; it is commonly found in metamorphic mountain belts worldwide. A small, ordinary specimen like this is typically worth about $1–$10, depending on provenance and appearance.
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