
metamorphic
Rounded quartzite pebble
Quartzite, composed predominantly of quartz (SiO₂)
AI-generated identification · may be incorrectThe smooth, rounded pebble is pale tan-gray with a subtly sparkly, granular surface. Quartz has Mohs hardness 7, vitreous-to-sugary luster, and trigonal crystal structure; individual grains are too small to identify confidently from the image.
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Physical properties
The smooth, rounded pebble is pale tan-gray with a subtly sparkly, granular surface. Quartz has Mohs hardness 7, vitreous-to-sugary luster, and trigonal crystal structure; individual grains are too small to identify confidently from the image.
Formation & geological history
Quartz-rich sandstone recrystallizes under heat and pressure into interlocking quartz grains. Quartzite forms in metamorphic terrains across many geological ages; this pebble’s age and source cannot be determined visually.
Uses & applications
Quartzite is used as crushed stone, building and decorative stone, and occasionally for lapidary work. This small pebble is mainly suitable for collecting or display.
Geological facts
Quartzite is generally harder and more resistant to weathering than its sandstone precursor. Its rounded shape likely reflects transport and abrasion in a stream or shoreline environment.
Field identification & locations
Look for a hard, quartz-rich rock with a sugary sparkle and grains that resist scratching by a steel knife; rounded edges suggest transport. Quartzite occurs worldwide, especially in mountain belts and river gravels.
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