Rock Identifier
Light-colored rounded pebble, likely quartzite (Quartzite, composed predominantly of quartz (SiO₂); identification is tentative from the image) — metamorphic
metamorphic

Light-colored rounded pebble, likely quartzite

Quartzite, composed predominantly of quartz (SiO₂); identification is tentative from the image

AI-generated identification · may be incorrect

Creamy beige, fine-grained and matte, with a rounded, water-worn shape. Quartz has Mohs hardness 7 and a trigonal crystal structure, but individual grains and cleavage are not discernible here.

Identified More metamorphic →
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Physical properties

Creamy beige, fine-grained and matte, with a rounded, water-worn shape. Quartz has Mohs hardness 7 and a trigonal crystal structure, but individual grains and cleavage are not discernible here.

Formation & geological history

Quartzite forms when quartz-rich sandstone is recrystallized by heat and pressure; its age depends on the source rock and metamorphic event. The pebble’s smoothness suggests transport and abrasion by water or sediment.

Uses & applications

Small pebbles are mainly used for landscaping, crafts, or collecting; quartzite is also used as decorative and construction stone.

Geological facts

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

Field identification & locations

A pale, dense pebble with a sugary or fused-grain texture may be quartzite; a close view or hardness test would help distinguish it from other light-colored rocks. Quartzite occurs worldwide in metamorphic terrains and river or beach gravels.