
metamorphic
Polished brown river pebble
Likely quartzite or weathered metabasalt; exact identification requires hardness and streak tests
AI-generated identification · may be incorrectFine-grained, rounded, brown-tan stone with dark green-black bands or inclusions and a polished/wet luster. Likely hardness 6–7 Mohs, nonmetallic, with no visible cleavage; composition may include quartz, feldspar, and dark amphibole or chlorite.
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Physical properties
Fine-grained, rounded, brown-tan stone with dark green-black bands or inclusions and a polished/wet luster. Likely hardness 6–7 Mohs, nonmetallic, with no visible cleavage; composition may include quartz, feldspar, and dark amphibole or chlorite.
Formation & geological history
Probably a naturally water-rounded cobble later polished or naturally smoothed by abrasion. If quartzite, it formed by metamorphism of sandstone; if metabasalt, it formed from altered volcanic rock, generally during Precambrian–Phanerozoic geological events.
Uses & applications
Suitable as a decorative pebble, paperweight, lapidary cabochon, or craft material; not distinctive enough for high-value jewelry or construction stone.
Geological facts
The image alone cannot reliably distinguish quartzite from basalt, schist, or another fine-grained metamorphic rock. A glass-scratch test and examination of a fresh edge would substantially improve identification.
Field identification & locations
Common in river gravels, glacial deposits, beaches, and landscaping stone collections. Quartzite should scratch glass and resist steel; basaltic material is usually dark, denser, and may show tiny feldspar crystals.
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