
mineral
Quartz (Water-worn pebble)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Translucent white to pale tan; Luster: Vitreous to waxy; Crystal Structure: Trigonal (though rounded here); Cleavage: None (conchoidal fracture).
- Hardness
- 7 on Mohs scale
- Color
- Translucent white to pale tan
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 on Mohs scale; Color: Translucent white to pale tan; Luster: Vitreous to waxy; Crystal Structure: Trigonal (though rounded here); Cleavage: None (conchoidal fracture).
Formation & geological history
Formed through hydrothermal processes or igneous crystallization, then subsequently weathered and smoothed by water action in a river, stream, or beach environment over thousands of years.
Uses & applications
Collecting, decorative vase filler, landscaping, or as a source of silica in glass manufacturing if found in high purity/volume.
Geological facts
Quartz is one of the most abundant minerals on Earth. River-tumbled pebbles like this one are nature's version of a rock tumbler, creating smooth surfaces through constant friction with water and silt.
Field identification & locations
Identify by its ability to scratch glass and its lack of cleavage. Common in alluvial deposits worldwide. Look for a translucent 'glow' when held against light.
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Other mineral specimens
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