
metamorphic
Light-colored rounded pebble, likely quartzite
Quartzite, composed predominantly of quartz (SiO₂); identification is tentative from the image
AI-generated identification · may be incorrectCreamy 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.
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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.
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