
mineral
Quartz Pebble
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Tan, off-white, and semi-translucent; Luster: Vitreous to waxy (when wet/polished); Crystal structure: Hexagonal (trigonal); Cleavage: None/Conchoidal fracture; Specific gravity: 2.65.
- Hardness
- 7 (Mohs scale)
- Color
- Tan, off-white, and semi-translucent
- Luster
- Vitreous to waxy (when wet/polished)
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Physical properties
Hardness: 7 (Mohs scale); Color: Tan, off-white, and semi-translucent; Luster: Vitreous to waxy (when wet/polished); Crystal structure: Hexagonal (trigonal); Cleavage: None/Conchoidal fracture; Specific gravity: 2.65.
Formation & geological history
Formed from hydrothermal veins or as a major constituent of igneous rocks. This specific specimen is a water-worn river pebble, shaped by erosion over thousands of years as it was transported by water.
Uses & applications
Commonly used as abrasive blasting material, in glass manufacturing, as a decorative landscape garden stone, and as a popular find for beginner rockhounds.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Its name comes from the German word 'Quarz', which had its origins in Slavic and West Slavonic words meaning 'hard'.
Field identification & locations
Identify in the field by its inability to be scratched by a steel knife and its lack of cleavage. Look for smooth, rounded textures in riverbeds, beaches, and glacial till. Common worldwide.
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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
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
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