Rock Identifier
Rounded quartzite cobble (Quartzite, composed predominantly of recrystallized quartz (SiO₂)) — metamorphic
metamorphic

Rounded quartzite cobble

Quartzite, composed predominantly of recrystallized quartz (SiO₂)

AI-generated identification · may be incorrect

Hardness about 7 Mohs; pale gray-white with rusty pink-brown iron-oxide staining, a dull to sugary sparkle, and no obvious cleavage. Quartz grains are interlocked in a massive texture; the smooth shape is from natural abrasion or tumbling.

Identified More metamorphic →
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Physical properties

Hardness about 7 Mohs; pale gray-white with rusty pink-brown iron-oxide staining, a dull to sugary sparkle, and no obvious cleavage. Quartz grains are interlocked in a massive texture; the smooth shape is from natural abrasion or tumbling.

Formation & geological history

Forms when quartz-rich sandstone is recrystallized by heat and pressure, commonly during regional metamorphism. The specimen’s specific age and source cannot be determined from the image.

Uses & applications

Used as decorative stone, landscaping gravel, building aggregate, and sometimes as a lapidary material.

Geological facts

Quartzite is generally harder and more resistant to weathering than its sandstone precursor.

Field identification & locations

Look for a dense, hard rock with interlocking quartz grains; it typically scratches glass and does not split readily along bedding. Quartzite occurs worldwide in metamorphic terrains and river or beach gravels.