
mineral
Quartz Pebble
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Off-white, yellowish-tan; Luster: Waxy to vitreous; Crystal structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Off-white, yellowish-tan
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: Off-white, yellowish-tan; Luster: Waxy to vitreous; Crystal structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed via igneous or hydrothermal processes and then weathered and rounded by water transport in a river or beach environment over thousands of years.
Uses & applications
Commonly used in landscaping, as a component in glass manufacturing, or as grit in industrial polishing and construction aggregates.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. This specimen is a 'river rock' variety, smoothed by natural erosion.
Field identification & locations
Identify by its hardness (cannot be scratched by a steel knife) and its smooth, rounded texture typical of fluvial deposits. Found globally in riverbeds and coastal regions.
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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