
mineral
White Quartz Pebble
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Milky white to translucent; Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Milky white to translucent
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 on Mohs scale; Color: Milky white to translucent; Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed from silica-rich hydrothermal solutions or as a primary constituent in igneous rocks like granite. This specific rounded shape is the result of mechanical weathering and river or coastal erosion over a geological period.
Uses & applications
Used in landscaping, as an abrasive, in glass manufacturing, for silicon production, and as decorative river stones or pocket stones.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Milky quartz gets its white appearance from tiny fluid inclusions of gas or liquid trapped during crystal growth.
Field identification & locations
Identify by its ability to scratch glass and steel, its lack of cleavage, and smooth, water-worn surface. Found globally in riverbeds, beaches, and glacial deposits.
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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