
metamorphic
Rounded river cobble, likely quartzite
Quartzite (chiefly recrystallized quartz, SiO₂); exact identification is uncertain from the image
AI-generated identification · may be incorrectSmooth, rounded, tan-brown surface with a fine-grained appearance; quartzite is typically Mohs 7, vitreous to dull, and has no cleavage. The wet surface and lack of a visible fresh fracture obscure diagnostic texture.
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Physical properties
Smooth, rounded, tan-brown surface with a fine-grained appearance; quartzite is typically Mohs 7, vitreous to dull, and has no cleavage. The wet surface and lack of a visible fresh fracture obscure diagnostic texture.
Formation & geological history
If quartzite, it formed when quartz-rich sandstone was metamorphosed under heat and pressure; its age depends on the source formation. The rounded shape indicates prolonged transport and abrasion in water.
Uses & applications
Quartzite is used as aggregate, paving and building stone, and sometimes as a decorative stone; this cobble is primarily a natural specimen.
Geological facts
The image shows a single cobble on a gravel bed, but color and shape alone cannot reliably distinguish quartzite from other hard rocks such as sandstone or fine-grained igneous rock.
Field identification & locations
Look for fused, interlocking quartz grains on a fresh break and test hardness: quartzite generally scratches glass. River gravels worldwide commonly contain rounded cobbles of many rock types.
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