
mineral
Rounded quartz-rich pebble
Likely microcrystalline quartz (chalcedony), possibly weathered quartzite
AI-generated identification · may be incorrectOpaque gray-brown, weakly translucent edges, dull to waxy luster, and irregular granular texture; quartz hardness is about 7 Mohs, with no cleavage and conchoidal fracture. The dark surface patches may be iron/manganese staining or attached matrix.
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Physical properties
Opaque gray-brown, weakly translucent edges, dull to waxy luster, and irregular granular texture; quartz hardness is about 7 Mohs, with no cleavage and conchoidal fracture. The dark surface patches may be iron/manganese staining or attached matrix.
Formation & geological history
Likely formed as silica-rich material in a vein, volcanic setting, or metamorphic rock, then rounded by stream or beach abrasion; its exact geological age and identity cannot be established from the photograph alone.
Uses & applications
Common material has little commercial value, but attractive chalcedony and quartzite are used for cabochons, carvings, ornaments, and occasionally aggregate or building stone.
Geological facts
Chalcedony is fibrous microcrystalline quartz, while quartzite is metamorphosed sandstone; both can look similar when weathered and rounded.
Field identification & locations
Test an inconspicuous spot with a steel file: quartz-rich material should resist scratching, while glassy streaks or softer surfaces suggest another rock. Commonly found in stream gravels, beaches, and weathered vein deposits.
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