Rock Identifier
Rounded quartz-rich cobble, likely quartzite (Quartzite; predominantly microcrystalline quartz (SiO₂), possibly with minor iron-oxide staining) — metamorphic
metamorphic

Rounded quartz-rich cobble, likely quartzite

Quartzite; predominantly microcrystalline quartz (SiO₂), possibly with minor iron-oxide staining

AI-generated identification · may be incorrect

Hardness about 7 Mohs; gray-brown to mauve color, weathered matte-to-slightly silky luster, massive granular texture, and no obvious cleavage. Its rounded shape and smooth surface indicate stream or beach abrasion rather than crystal form.

Identified More metamorphic
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Physical properties

Hardness about 7 Mohs; gray-brown to mauve color, weathered matte-to-slightly silky luster, massive granular texture, and no obvious cleavage. Its rounded shape and smooth surface indicate stream or beach abrasion rather than crystal form.

Formation & geological history

Quartzite forms when quartz-rich sandstone is recrystallized under heat and pressure during regional metamorphism; its age depends on the source formation and cannot be determined from the image. It commonly survives erosion as resistant cobbles.

Uses & applications

Used as crushed stone, aggregate, road material, building stone, countertops, and decorative landscaping rock; attractive pieces may be collected or polished.

Geological facts

Quartzite is generally harder and more resistant to weathering than sandstone. The mauve tint may result from iron oxides or minor accessory minerals.

Field identification & locations

Identify it by testing for quartz-like hardness: it should scratch ordinary glass, lack visible sand grains or bedding, and show interlocking grains on a fresh break. Common in metamorphic mountain belts and gravel deposits.