
mineral
Tumbled quartz-rich pebble, possibly rose quartz or quartzite
Quartz (SiO₂), potentially quartzite if composed of fused quartz grains
AI-generated identification · may be incorrectSmall rounded, matte-to-waxy specimen with pale pink, cream, and gray coloration; likely Mohs hardness 7, vitreous when freshly broken, with no obvious cleavage and conchoidal fracture. The image is insufficient to confirm crystal structure or specific gravity.
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Physical properties
Small rounded, matte-to-waxy specimen with pale pink, cream, and gray coloration; likely Mohs hardness 7, vitreous when freshly broken, with no obvious cleavage and conchoidal fracture. The image is insufficient to confirm crystal structure or specific gravity.
Formation & geological history
Quartz forms in igneous, metamorphic, and hydrothermal settings; quartzite forms when sandstone is metamorphosed. Its rounded shape indicates stream abrasion or human tumbling; age cannot be determined from the image.
Uses & applications
Used for lapidary items, carvings, jewelry, countertops, glass, and industrial silica. As a small common pebble, it has modest collector value.
Geological facts
Pink color may result from trace iron, inclusions, or radiation-related defects, but appearance alone cannot distinguish rose quartz from pale quartzite.
Field identification & locations
Common in quartz-bearing gravels and metamorphic terrains worldwide. Test with a steel file or glass: true quartz should scratch glass and resist a steel knife; inspect a fresh surface for granular quartzite texture.
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Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary