
mineral
Milky Quartz Pebble
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: White to translucent; Luster: Vitreous/greasy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 (Mohs scale)
- Color
- White to translucent
- Luster
- Vitreous/greasy
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Physical properties
Hardness: 7 (Mohs scale); Color: White to translucent; Luster: Vitreous/greasy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed from the crystallization of silica-rich hydrothermal fluids in veins or as a primary constituent in igneous rocks like granite. This specimen has been rounded by fluvial (river) or coastal erosion.
Uses & applications
Used in glass manufacturing, electronics (piezoelectric properties), abrasives, and as decorative landscaping stone or tumbled pocket stones.
Geological facts
Milky quartz gets its cloudy appearance from minute fluid inclusions of gas or liquid trapped during the crystal's growth. It is the most common variety of crystalline quartz on Earth.
Field identification & locations
Identify in the field by its hardness (it will scratch glass), lack of cleavage, and waxy luster when wet. Commonly found in riverbeds, glacial tills, and beaches 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
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