
mineral
Quartz Pebble
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Milky white to translucent with some yellowish oxidation; Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal (though water-worn); Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Milky white to translucent with some yellowish oxidation
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 (Mohs scale); Color: Milky white to translucent with some yellowish oxidation; Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal (though water-worn); Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed through the cooling of silica-rich magma or from hydrothermal veins. This specific specimen has been rounded by fluvial processes (water erosion) and is likely part of a quaternary sedimentary deposit.
Uses & applications
Used in glassmaking, electronics, abrasives, and common landscaping gravel. High-purity quartz is used for silicon wafers in technology.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. It is piezoelectric, meaning it generates an electric charge in response to applied mechanical stress.
Field identification & locations
Identify in the field by its hardness (it will scratch glass) and lack of cleavage. Commonly found in riverbeds, beaches, and glacial till globally.
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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