Rock Identifier
Rounded river cobble, likely quartzite (Quartzite (chiefly recrystallized quartz, SiO₂); exact identification is uncertain from the image) — metamorphic
metamorphic

Rounded river cobble, likely quartzite

Quartzite (chiefly recrystallized quartz, SiO₂); exact identification is uncertain from the image

AI-generated identification · may be incorrect

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.

Identified More metamorphic →
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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.