
metamorphic
Pink quartzite pebble
Quartzite, composed predominantly of quartz (SiO₂)
AI-generated identification · may be incorrectPale pink to salmon, dull to slightly vitreous surface; quartz hardness is 7 Mohs. The image does not reveal crystal structure or cleavage; quartzite typically has interlocking quartz grains and no distinct cleavage.
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Physical properties
Pale pink to salmon, dull to slightly vitreous surface; quartz hardness is 7 Mohs. The image does not reveal crystal structure or cleavage; quartzite typically has interlocking quartz grains and no distinct cleavage.
Formation & geological history
Formed when quartz-rich sandstone was recrystallized by heat and pressure, usually during regional metamorphism. Its age cannot be determined from the photograph.
Uses & applications
Quartzite is used as crushed stone, paving and building stone; attractive pieces may be collected or used decoratively.
Geological facts
Pink coloration commonly comes from trace iron-bearing minerals or inclusions, rather than pink quartz alone.
Field identification & locations
A hard, quartz-rich pebble with a granular texture and no obvious layering supports quartzite identification; similar-looking pink rocks can be difficult to distinguish from the image alone. Quartzite occurs worldwide wherever quartz sandstone has been metamorphosed.
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