Rock Identifier
Rounded quartz-rich pebble (Likely quartzite, composed chiefly of SiO₂ (quartz); identification is uncertain from the photograph) — igneous
igneous

Rounded quartz-rich pebble

Likely quartzite, composed chiefly of SiO₂ (quartz); identification is uncertain from the photograph

AI-generated identification · may be incorrect

Pale gray-white, rounded and weathered, with a granular/sugary surface and slight sparkle. Quartz hardness is 7 Mohs, vitreous luster, and trigonal crystal structure; quartzite has no cleavage and typically breaks irregularly.

Identified More igneous →
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Physical properties

Pale gray-white, rounded and weathered, with a granular/sugary surface and slight sparkle. Quartz hardness is 7 Mohs, vitreous luster, and trigonal crystal structure; quartzite has no cleavage and typically breaks irregularly.

Formation & geological history

If quartzite, it formed when quartz sandstone was metamorphosed under heat and pressure, then was rounded by water or other erosion. Its age and source cannot be determined from the image.

Uses & applications

Small pebbles are commonly used for collecting, landscaping, and decorative crafts; quartzite is also used as construction aggregate and dimension stone.

Geological facts

Quartzite’s interlocking quartz grains make it hard and resistant to weathering. A simple scratch test against glass can help distinguish it from softer rocks, though it is not conclusive.

Field identification & locations

Look for a hard, quartz-rich texture and grains that appear fused rather than loosely cemented; rounded pebbles occur in riverbeds, beaches, and glacial deposits worldwide.